This document contains information on lithology, alteration, mineralization, and breccias observed in geological samples and outcrops. It provides coded designations for different rock types, alteration styles, minerals, textures, and other features. The codes can be used to concisely describe and record lithological data in exploration and mining projects.
Sedimentary structures provide important information about the depositional environment and post-depositional changes to sedimentary rocks. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding reflecting currents, load casts and flame structures from density differences, sole structures on bed bases indicating erosion, and trace fossils providing evidence of organism behavior and helping determine correct bed orientations. Together, an understanding of these sedimentary structures allows reconstruction of the depositional environment and testing of the law of superposition.
All Igneous rock textures with examples in easy and simple way to understand and increase microscopic studies skills and the way to easily identify igneous rocks under polarized microscope.
Batuan sedimen klastik terbentuk dari proses pelapukan, erosi, transportasi, dan pengendapan fragmen batuan. Terdiri dari butiran klastik seperti kuarsa, feldspar, dan fragmen litik serta matriks lempung. Diklasifikasi berdasarkan ukuran butir, komposisi, dan struktur perlapisan seperti laminasi. Contohnya adalah batupasir, konglomerat, dan mudrock.
The document summarizes a seminar on subduction and abduction zones. It defines subduction as the process where one tectonic plate moves under another at a convergent boundary. Abduction is the overthrusting of oceanic crust onto continental crust at these boundaries. The document describes different types of abduction mechanisms including upwedging in subduction zones, compressional telescoping onto continental margins, and abduction occurring during continental collisions when oceanic crust is trapped between converging continents.
Understanding the sedimentary rocks - Geotalk 2 (MGSS)KYI KHIN
Ìý
Sedimentary rocks form from the compaction and cementation of sediments like sand and mud. This document discusses the formation of sedimentary rocks, including weathering, erosion, transportation, deposition, and diagenesis. It describes key sedimentary rock types like sandstone, shale, and conglomerate. Examples are given of each rock type and how to identify them based on composition, texture, and sedimentary structures. The study of sedimentary rocks provides information about geology, natural resources, and earth's history.
Sequence stratigraphy involves subdividing stratigraphic records based on bounding discontinuities. A depositional sequence is defined as a succession of genetically related strata bounded by unconformities and correlative conformities. During a sequence, systems tracts are deposited in response to changes in relative sea level, including highstand, falling stage, lowstand, and transgressive tracts bounded by surfaces like sequence boundaries, transgressive surfaces, and flooding surfaces.
Climbing ripple laminations are formed by the superimposition of migrating ripples where deposition occurs rapidly during ripple migration, causing the ripples to climb upon one another rather than migrate laterally. They are classified based on the angle of climbing relative to the stoss side angle, and form under conditions of abundant suspended sediment supply and rapid burial, preserving the original rippled layers. Climbing ripples indicate deposition exceeded migration and are found in environments with high sedimentation rates like river floodplains, point bars, and deltas.
This document discusses iron ore and its mineralogy, types of iron formations, distribution, and uses. It notes that iron is the second most abundant element in the earth's crust and accounts for 5-6% of the lithosphere. There are two main types of iron formations - the Algoma type which is associated with volcanic and greywacke sediments, and the Superior type which is characteristic of Proterozoic formations. The major deposits of iron ore are located in India in the states of Jharkhand, Orissa, Chattisgarh, Karnataka, Maharashtra, Andhra Pradesh, and Goa. Iron has been widely used since ancient times in construction, infrastructure, appliances and buildings.
The document describes a petrographic study of rocks in the Vallanadu area of Tamil Nadu, India. It finds that the main rock types in the area are charnockites, khondalites, cordierite gneisses, calc-silicate rocks, and grey and pink granites. Two sets of conjugate shear systems are observed, including a NW-SE dextral shear zone conjugating with a NE-SW sinistral zone. Granites in the area formed syntectonically. The Vallanadu area experienced initial ductile deformation followed by brittle-ductile deformation during the Neoproterozoic to Cambrian period.
The document provides an outline for a series of lectures on metals, minerals, mining and environmental problems. It discusses various topics including ore mineralogy, mining methods, ore processing, waste management, and environmental and social concerns. Specific problems examined include surface subsidence from underground mining, rockbursts, tailings dam failures, cyanidation wastes, radioactive wastes, and acid mine drainage. The document also provides background information on elements, minerals, rock types, and ore deposit geology.
The document discusses the vertebrate fossils found in the Siwalik region between 16-5 million years ago. It provides details on the lithostratigraphy and chronostratigraphy of the Siwalik Group, which is divided into Upper, Middle, and Lower Siwalik. During the early Miocene climate was warm and humid, supporting a variety of large mammals. Beginning around 11.5 million years ago, the climate started becoming more arid and open grasslands expanded, attracting different herbivorous and grazing mammals. By the late Miocene/Pliocene between 5-2 million years ago, a savannah environment dominated and fauna included early humans, horses, rhinos, giraffes
In the Environmental Sciences Isotope geochemistry has become an essential tool for the
environmental sciences, providing clearly defined tracers of sources, quantitative information
on mixing, identification of physical and chemical processes, and information on the rates of
environmental processes. Clearly, this tool will continue to be important in all aspects of the
field, including studies of contamination, resource management, climate change, bio-
geochemistry, exploration geochemistry, archaeology, and ecology. In addition to further
utilization of established methods, new applications will continue to be developed.
A sedimentary facies is a body of rock or sediment that is characterized by particular attributes that distinguish it from adjacent rock bodies. These attributes include lithology, color, texture, sedimentary structures, mineral/fossil content, and bed geometry. Together these attributes provide clues about the depositional environment. Different facies reflect different environments, such as beach/shallow marine facies indicating sandstone and offshore marine facies indicating shale. Facies analysis studies these attributes to interpret depositional environments and geological history at various scales.
This document discusses minerals and their properties. It defines minerals as natural, inorganic solids with an internal atomic structure and definite chemical composition. Minerals are composed of elements, whose atoms bond together through ionic, covalent, or metallic bonds. The document outlines several key mineral groups including silicates, oxides, sulfides, carbonates, and halides. It notes that silicates are the most abundant mineral group in the Earth's crust and describes their tetrahedral structures. The document also discusses physical properties of minerals like hardness, luster, and cleavage. Finally, it distinguishes between renewable and nonrenewable natural resources, with minerals being nonrenewable.
The document provides information on the textures of igneous rocks. It defines texture as the size, shape, and arrangement of mineral grains in a rock. Primary textures form during the cooling and solidification of magma, influenced by the rates of nucleation, crystal growth, and diffusion. Secondary textures form after the rock has completely solidified. Common primary textures include phaneric, porphyritic, and inequigranular textures which depend on the cooling rate. Compositional zoning and cumulate textures are also described.
This document defines folds and describes their key elements and classification. Folds are shapes or volume changes in rock layers caused by deformation. They indicate stress and can be described geometrically. Folds are classified based on attributes like their interlimb angle, symmetry, position, and isogon characteristics. Gentle folds have interlimb angles from 180 to 120 degrees, while tight folds are from 30 to 0 degrees. Symmetric folds have symmetry planes, while asymmetric folds are monoclinal. Anticlines fold upwards and synclines fold downwards. The document also discusses methods for constructing fold profiles.
The document discusses the silicate group of minerals, which are an important class of rock-forming minerals. It describes the chemical composition, atomic structure, and classification of silicates. Silicates are made up of silicon-oxygen tetrahedra that are linked together in different ways, forming independent tetrahedra, double linked tetrahedra, complex linked tetrahedra, chains, sheets, and networks. The document also discusses specific silicate mineral groups like felspars and pyroxenes, providing details on their composition, structure, and properties.
This document provides an overview of palaeontology and discusses fossils of gastropods. It defines palaeontology as the study of ancient life and describes the different types of fossil preservation including entire body, entire skeleton, petrification, molds and casts, imprints, and traces. It outlines the importance of fossils for studying evolution, paleoecology, and paleogeography. The document then focuses on invertebrate palaeontology, describing the morphology and taxonomy of gastropods. Key gastropod fossils discussed include species that have existed from the Paleozoic to present.
Este informe describe la determinación del pH en diferentes tipos de arcillas, incluyendo San Marcos, Sinincay, Astillado y Ball Clay. Los resultados mostraron que la arcilla San Marcos tenÃa un pH alcalino de 7.726, mientras que las otras tres arcillas tenÃan pH ácidos entre 4.62 y 5.132. El pH de las arcillas depende de su composición mineralógica y afecta sus propiedades como la capacidad de floculación, trabajabilidad y capacidad de intercambio catiónico. La medición del pH es importante para comprender el
Equipos De Muestreo Metalúrgico Heath & SherwoodFabian Perez
Ìý
Los equipos de H&S son diseñados con base en recomendaciones por los consultores de muestreo y con base en el Código AMIRA P754 de buenas prácticas para el conteo metalúrgico y el muestreo representativo, es por ello que son reconocidos a nivel mundial.
Texture of Ore Minerals; Importance of Studying Textures; Individual Grains Properties; Filling of voids; Texture Types; Genetically differentiated between Texture types; Secondary textures from replacement; Hypogene Texture; Supergene Texture; Primary texture formed from Melts; Primary texture of open-space deposition; Secondary textures from cooling; Secondary textures from deformation; TEXTURES OF ECONOMIC ORE DEPOSITS; Textures of Magmatic ores; Cumulus textures; Intergranular or intercumulus textures; Exsolution textures; Textures of hydrothermal ore deposits and skarns; Replacement textures; Open space filling textures; Textures characteristic of surfacial or near surface environments and processes; Criteria for identifying replacement textures; Vein and Veining have different Nature Features
This document provides information about the classification and characteristics of limestone and sandstone. It begins by defining limestone as a sedimentary rock composed mainly of calcium carbonate in the form of calcite and aragonite. It describes the microscopic components of limestone including skeletal fragments, ooids, peloids, and lime mud. It explains that limestone forms most readily in warm, shallow marine environments. The document then discusses various types of limestone based on composition and texture. It concludes by outlining some of the major uses of limestone, particularly in construction as a crushed stone for concrete, cement production, and road base. The document also provides definitions of quartz arenites, feldspathic arenites, and lith
This document summarizes igneous petrology and the structure and composition of the Earth's interior. It discusses how the Earth is composed of layers including the crust, mantle, outer core, and inner core. The crust is divided into oceanic and continental crust. The mantle makes up most of the Earth's volume and is composed of ultramafic rock. Heat transfer mechanisms like conduction, convection, and advection are described. The geothermal gradient and how temperature increases with depth is also summarized. Plate tectonics and mantle convection are driving the dynamic cooling of the Earth.
Carbonates are produced in shallow, sunlit seas through direct or biologically mediated precipitation of calcium carbonate. Carbonate platforms accumulate vast amounts of sediment and come in various forms like ramps, shelves, banks, and epeiric platforms. Carbonate production and platform morphology are influenced by factors such as climate, oceanography, tectonics, and sea level change. Carbonate platforms exhibit various facies and vertical successions that reflect the interplay between energy levels, morphology, and sea level fluctuations. Common buildups within platforms include reefs, mounds, bioherms, and biostromes formed by organisms trapping and binding sediment.
This document provides an overview of petrology and the classification of rocks. It discusses the three main types of rocks - igneous, metamorphic, and sedimentary rocks. For each rock type, it describes their origin and formation processes. It also discusses various rock properties such as texture, structure, and mineral composition. The document emphasizes the importance of petrology for civil engineering applications when constructing with and building on various rock formations.
Igneous rocks can have several different structures depending on how the magma solidifies. These structures include vesicular, amygdoidal, block lava, ropy lava, and pillow structures. Vesicular structures form when gases escape from cooling lava, leaving cavities called vesicles. Amygdoidal structures occur when vesicles become filled with secondary minerals after formation. Block lava has a rough, angular texture from slow cooling of viscous lava. Ropy lava has a wrinkled but smooth surface from the rapid cooling of less viscous lava. Pillow structures are bulbous and overlapping shapes that form when lava solidifies under water.
Alat-alat yang digunakan dalam pengolahan pasir besi meliputi belt conveyor, trommel screen, magnetic drum separator, dan humprey spiral. Tahapan pengolahannya terdiri dari pemisahan pasir besi dan pengotor, pemisahan konsentrat dan tailing menggunakan magnetic drum separator berbeda gauss, hingga diperoleh konsentrat magnetite dan ilmenite serta tailing vanadinite, hematite, dan kuarsa.
Objective Capital's Global Resources Investment Forum 2012
Ironmongers' Hall, City of London
25 September 2012
Speaker: Richard Williams, Helio Resource
The document describes a petrographic study of rocks in the Vallanadu area of Tamil Nadu, India. It finds that the main rock types in the area are charnockites, khondalites, cordierite gneisses, calc-silicate rocks, and grey and pink granites. Two sets of conjugate shear systems are observed, including a NW-SE dextral shear zone conjugating with a NE-SW sinistral zone. Granites in the area formed syntectonically. The Vallanadu area experienced initial ductile deformation followed by brittle-ductile deformation during the Neoproterozoic to Cambrian period.
The document provides an outline for a series of lectures on metals, minerals, mining and environmental problems. It discusses various topics including ore mineralogy, mining methods, ore processing, waste management, and environmental and social concerns. Specific problems examined include surface subsidence from underground mining, rockbursts, tailings dam failures, cyanidation wastes, radioactive wastes, and acid mine drainage. The document also provides background information on elements, minerals, rock types, and ore deposit geology.
The document discusses the vertebrate fossils found in the Siwalik region between 16-5 million years ago. It provides details on the lithostratigraphy and chronostratigraphy of the Siwalik Group, which is divided into Upper, Middle, and Lower Siwalik. During the early Miocene climate was warm and humid, supporting a variety of large mammals. Beginning around 11.5 million years ago, the climate started becoming more arid and open grasslands expanded, attracting different herbivorous and grazing mammals. By the late Miocene/Pliocene between 5-2 million years ago, a savannah environment dominated and fauna included early humans, horses, rhinos, giraffes
In the Environmental Sciences Isotope geochemistry has become an essential tool for the
environmental sciences, providing clearly defined tracers of sources, quantitative information
on mixing, identification of physical and chemical processes, and information on the rates of
environmental processes. Clearly, this tool will continue to be important in all aspects of the
field, including studies of contamination, resource management, climate change, bio-
geochemistry, exploration geochemistry, archaeology, and ecology. In addition to further
utilization of established methods, new applications will continue to be developed.
A sedimentary facies is a body of rock or sediment that is characterized by particular attributes that distinguish it from adjacent rock bodies. These attributes include lithology, color, texture, sedimentary structures, mineral/fossil content, and bed geometry. Together these attributes provide clues about the depositional environment. Different facies reflect different environments, such as beach/shallow marine facies indicating sandstone and offshore marine facies indicating shale. Facies analysis studies these attributes to interpret depositional environments and geological history at various scales.
This document discusses minerals and their properties. It defines minerals as natural, inorganic solids with an internal atomic structure and definite chemical composition. Minerals are composed of elements, whose atoms bond together through ionic, covalent, or metallic bonds. The document outlines several key mineral groups including silicates, oxides, sulfides, carbonates, and halides. It notes that silicates are the most abundant mineral group in the Earth's crust and describes their tetrahedral structures. The document also discusses physical properties of minerals like hardness, luster, and cleavage. Finally, it distinguishes between renewable and nonrenewable natural resources, with minerals being nonrenewable.
The document provides information on the textures of igneous rocks. It defines texture as the size, shape, and arrangement of mineral grains in a rock. Primary textures form during the cooling and solidification of magma, influenced by the rates of nucleation, crystal growth, and diffusion. Secondary textures form after the rock has completely solidified. Common primary textures include phaneric, porphyritic, and inequigranular textures which depend on the cooling rate. Compositional zoning and cumulate textures are also described.
This document defines folds and describes their key elements and classification. Folds are shapes or volume changes in rock layers caused by deformation. They indicate stress and can be described geometrically. Folds are classified based on attributes like their interlimb angle, symmetry, position, and isogon characteristics. Gentle folds have interlimb angles from 180 to 120 degrees, while tight folds are from 30 to 0 degrees. Symmetric folds have symmetry planes, while asymmetric folds are monoclinal. Anticlines fold upwards and synclines fold downwards. The document also discusses methods for constructing fold profiles.
The document discusses the silicate group of minerals, which are an important class of rock-forming minerals. It describes the chemical composition, atomic structure, and classification of silicates. Silicates are made up of silicon-oxygen tetrahedra that are linked together in different ways, forming independent tetrahedra, double linked tetrahedra, complex linked tetrahedra, chains, sheets, and networks. The document also discusses specific silicate mineral groups like felspars and pyroxenes, providing details on their composition, structure, and properties.
This document provides an overview of palaeontology and discusses fossils of gastropods. It defines palaeontology as the study of ancient life and describes the different types of fossil preservation including entire body, entire skeleton, petrification, molds and casts, imprints, and traces. It outlines the importance of fossils for studying evolution, paleoecology, and paleogeography. The document then focuses on invertebrate palaeontology, describing the morphology and taxonomy of gastropods. Key gastropod fossils discussed include species that have existed from the Paleozoic to present.
Este informe describe la determinación del pH en diferentes tipos de arcillas, incluyendo San Marcos, Sinincay, Astillado y Ball Clay. Los resultados mostraron que la arcilla San Marcos tenÃa un pH alcalino de 7.726, mientras que las otras tres arcillas tenÃan pH ácidos entre 4.62 y 5.132. El pH de las arcillas depende de su composición mineralógica y afecta sus propiedades como la capacidad de floculación, trabajabilidad y capacidad de intercambio catiónico. La medición del pH es importante para comprender el
Equipos De Muestreo Metalúrgico Heath & SherwoodFabian Perez
Ìý
Los equipos de H&S son diseñados con base en recomendaciones por los consultores de muestreo y con base en el Código AMIRA P754 de buenas prácticas para el conteo metalúrgico y el muestreo representativo, es por ello que son reconocidos a nivel mundial.
Texture of Ore Minerals; Importance of Studying Textures; Individual Grains Properties; Filling of voids; Texture Types; Genetically differentiated between Texture types; Secondary textures from replacement; Hypogene Texture; Supergene Texture; Primary texture formed from Melts; Primary texture of open-space deposition; Secondary textures from cooling; Secondary textures from deformation; TEXTURES OF ECONOMIC ORE DEPOSITS; Textures of Magmatic ores; Cumulus textures; Intergranular or intercumulus textures; Exsolution textures; Textures of hydrothermal ore deposits and skarns; Replacement textures; Open space filling textures; Textures characteristic of surfacial or near surface environments and processes; Criteria for identifying replacement textures; Vein and Veining have different Nature Features
This document provides information about the classification and characteristics of limestone and sandstone. It begins by defining limestone as a sedimentary rock composed mainly of calcium carbonate in the form of calcite and aragonite. It describes the microscopic components of limestone including skeletal fragments, ooids, peloids, and lime mud. It explains that limestone forms most readily in warm, shallow marine environments. The document then discusses various types of limestone based on composition and texture. It concludes by outlining some of the major uses of limestone, particularly in construction as a crushed stone for concrete, cement production, and road base. The document also provides definitions of quartz arenites, feldspathic arenites, and lith
This document summarizes igneous petrology and the structure and composition of the Earth's interior. It discusses how the Earth is composed of layers including the crust, mantle, outer core, and inner core. The crust is divided into oceanic and continental crust. The mantle makes up most of the Earth's volume and is composed of ultramafic rock. Heat transfer mechanisms like conduction, convection, and advection are described. The geothermal gradient and how temperature increases with depth is also summarized. Plate tectonics and mantle convection are driving the dynamic cooling of the Earth.
Carbonates are produced in shallow, sunlit seas through direct or biologically mediated precipitation of calcium carbonate. Carbonate platforms accumulate vast amounts of sediment and come in various forms like ramps, shelves, banks, and epeiric platforms. Carbonate production and platform morphology are influenced by factors such as climate, oceanography, tectonics, and sea level change. Carbonate platforms exhibit various facies and vertical successions that reflect the interplay between energy levels, morphology, and sea level fluctuations. Common buildups within platforms include reefs, mounds, bioherms, and biostromes formed by organisms trapping and binding sediment.
This document provides an overview of petrology and the classification of rocks. It discusses the three main types of rocks - igneous, metamorphic, and sedimentary rocks. For each rock type, it describes their origin and formation processes. It also discusses various rock properties such as texture, structure, and mineral composition. The document emphasizes the importance of petrology for civil engineering applications when constructing with and building on various rock formations.
Igneous rocks can have several different structures depending on how the magma solidifies. These structures include vesicular, amygdoidal, block lava, ropy lava, and pillow structures. Vesicular structures form when gases escape from cooling lava, leaving cavities called vesicles. Amygdoidal structures occur when vesicles become filled with secondary minerals after formation. Block lava has a rough, angular texture from slow cooling of viscous lava. Ropy lava has a wrinkled but smooth surface from the rapid cooling of less viscous lava. Pillow structures are bulbous and overlapping shapes that form when lava solidifies under water.
Alat-alat yang digunakan dalam pengolahan pasir besi meliputi belt conveyor, trommel screen, magnetic drum separator, dan humprey spiral. Tahapan pengolahannya terdiri dari pemisahan pasir besi dan pengotor, pemisahan konsentrat dan tailing menggunakan magnetic drum separator berbeda gauss, hingga diperoleh konsentrat magnetite dan ilmenite serta tailing vanadinite, hematite, dan kuarsa.
Objective Capital's Global Resources Investment Forum 2012
Ironmongers' Hall, City of London
25 September 2012
Speaker: Richard Williams, Helio Resource
Andiamo Exploration is a private company exploring for gold and base metals in Eritrea. It has a 723 square km exploration license with multiple targets identified through geophysics and drilling. At its Yacob Dewar target, aircore and diamond drilling of an oxide gold cap returned intersections up to 5.7 g/t gold. Further reverse circulation and diamond drilling is testing the deeper sulphide potential and assays are expected in June 2012. Additional targets on the license including Adi Meriray have returned disseminated and massive sulphides in initial drilling.
Navigator Resources Limited Managing Director David Hatch presented at the Commonwealth Resources Investment Forum on May 22, 2012. The presentation summarized Navigator's two gold projects in Western Australia: Bronzewing and Leonora. At Bronzewing, mining operations are focused on expanding cutbacks at the Cockburn open pit, with forecasts of 78,000-96,000 ounces of gold production over 2012-2014. The Leonora project contains a 745,000 ounce gold resource across three areas that could support potential production of 50,000 ounces annually.
The document summarizes a presentation by Louis Coetzee, CEO of Kibo Mining, about Kibo's exploration activities in Tanzania. Kibo has acquired several projects in Tanzania prospective for gold, nickel, coal, and uranium. These include the Lake Victoria gold project, Morogoro project, Haneti project, and the Rukwa coal project. Kibo is also in the process of acquiring Mzuri Energy and Mayborn Investments, which would give it ownership of additional coal and uranium projects in southern Tanzania. The presentation compares Kibo's projects to other major mines and deposits in Tanzania and other countries to demonstrate the potential of its properties.
1. LITHOLOGY 1
Confidence Index - 1: positive 2: confident 3: probable 4: guess
pad fillPF
SURFICIAL DEPOSITS
gravelGr
perched gravelGrp
fluvial sedsFs alluviumAlv
glacial tillGlt screeSc
soilSo
conglomerateSCg
SSdb carb sandstone
SEDIMENTS (S)
SAr arkose
SSd sandstone
calc sandstoneSSdc
SSsc calc siltstone
SSs siltstone
SSsb carb siltstone
lamin siltstoneSSsl
SMsb carb mudstone
SMs mudstone
SMsf fer mudstone
calc mudstoneSMsc
SShg graphitic shale
SMsp peb mudstone
SSh shale
carb shaleSShb
SCl chalk
SGw greywake
SCh chert
limestoneSLs
SEv evaporite
SLso oolitic limestone
SLsc marly limestone
gneissMGn
MSk skarn
METAMORPHICS (M)
MHf hornfels
MMb marble
mt skarnMSKmt
MSkgtep gt-ep skarn
MSkmtgt mt-gt skarn
MSkgt gt skarn
ep skarnMSkep
MSksc sc skarn
MSkac ac skarn
MSkdp di skarn
meta basaltMVb
MSd meta sandstone
MMs meta mudstone
MSs meta siltstone
phylliteMPh
MShg green schist
MSh schist
MShp glauc schist
amphiboliteMSha
MHfp pyx hornfels
MShu granulite
MHfh hb hornfels
LITHOLOGY DATA RECORDING COLUMNS
LITH BXT BXC BXM %BM CI
S**
bxtype/facies
M**
bxclasts
V**
bxmatrix
I**
%bxmatrix
confidenceindex
IDY**
IDM**
IH**
IP**
sedimentary
metamorphic
volcanic
igneous
dyke
dome
hypabyssal
plutonic
glacial moraineGmor
r
clastrounding
SKE endoskarn
SKX exoskarn
OXIDATION STATE
Complete Oxidation
Strongly Oxidised
Moderately Oxidised
Weakly Oxidised
Trace Oxidation
Unoxidised
- no sulphides remaining
- trace Sx, strong FeO development
- approx 50% Sx oxidised
- most Sx preserved, signif FeO on partings
- trace FeO on partings, Sx
- fresh, no FeO, Sx
5
3
4
2
1
0
MINERAL EXPLORATION
Mine concentrate grab
DDH select
RCH composite
Open hole composite
Mine mill feedSoil pit BLEG
DDH composite
GEOLOGICAL REFERENCE CODES
Mine dump grab
Float Sample
Pit channel sample
Subcrop grab
Outcrop pannel
Outcrop grab
Outcrop channel
Outcrop chip
SAMPLE TYPE
SCGR
PTCH
OCPN
OCCH
OCRC
OCGR
FLGR
MIDP
Soil auger mesh
MIFD
SOAG
SOBL
OHCO
RCCO
DDSL
DDCO
MICO
Soil pit meshSOPT
Mobile metal ionSMMI
Underground Select
Underground channel
Underground chipUGRC
UGCH
UGSL
SSED BLEG
SSED meshSSMS
SSBL
S J MELDRUM
2016
PORPHYRY, SKARN & EPITHERMAL SYSTEMS
ver 6 / 2016
Calle las Tres Marias 363/6
Monterrico, Surco
Lima. Peru
CEL: ++51 19 9906 8514
meldrum.geo@gmail.com
SSED pan conSSPC
ferricreteFct
SLsd dirty LS
SLsh sinkhole fill
B bedded
SLd dolomite
SLsy shelly limestone
SVcl volcaniclastic
SFlch flysch seds
quartziteMQz
MMg migmatite
GB graded bedding
RB reverse bedding I indurated
CB cross bedded F fossiliferous
Features:
SNd sinter distal apr <35
SNn sinter near vent >60
SNs sinter mid slope <60
2. LITHOLOGY 2
VOLCANICS (V)
igneous designator
intrusive facies
composition
phenocrysts / crystals
textures
grain size
features
volcanic designator
composition
minerals (abundance order)
volc facies
grain size
features
COMPOSITION
D dacite
A andesite
rhyodaciteRD
R rhyolite
basaltB
BA basaltic andesite
P phonolite
TA trachyandesite
tephriteE
L latiteT trachyite
VOLCANIC FACIES
clt crystal lithic tuff
ct crystaltuff
lithic tufflt
ft pyroclastic flowtufft
at ash tuff
lpt accret lapilli tuff
vtt vitric tuff
fragmentalfgm
lhr lahar
ba block and ash
MINERALS
b biotite
h hornblende
pyroxenep
m magnetite
quartzq
f feldspar
GRAIN SIZE
fm fine to medium
mediumm
mc medium coarse
very finevf
f fine
c coarse
pillow basaltp
ign ignimbrite
FEATURES
VE vessicular
L leucocratic
W welded
flow bandedFB
D melanocratic
RB reverse graded bedded
GB graded bedded
EXAMPLES
VAct fhq D dark andesitic crystal tuff with feld hornblend and quartz crystals/phenos
VRDign fqh W welded rhyodacitic ignimbrite with feld & quartz phenos/crystals
EXTRACT AS MUCH INFORMATION IN A CODED FORM AS POSSIBLE
LITHOLOGY 3
INTRUSIVES (I)
INTRUSIVE FACIES
IP plutonicIH hypabyssaldykeIDY
IDM dome
pg pegmatite
gb gabbro
lamprophyrela
sp serpentenitemonzonitemz
mzg monzogabbro
sy syenite
pl aplite
COMMON MINERALS
b biotite
h hornblende
pyroxenep
m magnetite
quartzq
f feldspar
ROCK TEXTURES
PE porph > equigranularaphaniticA
PA porphyritic, aphanitic gmass equigranularE
P porphyritic
G graphictic
FEATURES
VE vessicular
L leucocratic FY feltyflow bandedFB
D melanocratic
COMPOSITION
an andesitic
dm microdiorite
daciticda
rd rhyodacitic
doleritedo
di diorite
gd granodiorite
g granitic
tonaliteto
rh rhyolitic
GRAIN SIZE
fm fine to medium
mediumm
mc medium coarsevery finevf
f fine c coarse
olivineo
a augite
VT vitric
ba basaltic andesite
EP equi > porphyritic
BRECCIA FACIES TABLE
BRECCIA FACIES TABLE CONTD
g glass DX
proximalPX
distal
FACIES
VI vitric
a augite
UT tephra
CR crystal crowded
fl lava flow
CR crystal crowded
3. BXi intrusion bx
BRECCIAS (BX)
BXf fault bx
BXt tectonic bx
jigsaw bxBXj
BXs pseudomicro bx
BXc crackle bx
BXp
phreatic bx
rock flour bxBXr
BXb pebble bx
BXrc rf-clastic bx
BXh hydrothermal bx
very angularva
CLAST ROUNDING (r)
an angular
sub-angularsa
sr sub-rounded
roundedro
wr well rounded
ploymictPL
BRECCIA CLASTS (BXC)
ML monolithic
meta sedsMS
IG igneous
porphyryPO
MM metamorphic
*** 'specified lithologies'
quartzqz
fe iron oxides
BRECCIA MATRIX (BXM)
qz-sx qz-sulphide
sx sulphide
qz-fe oxqz-fe
ja jarosite
qz-al qz-alunite
al alunite
qz-jarositeqz-ja
al-pf al-pyrophyllite
cl clay
pf pyrophyllite
OR - a lithology or other mineral species
LITHOLOGY 4
BXv volcanic bx
BXg phreatomagmatic
BXp
phreatic bx
BX9
BX1
BX4
BX3
BX6
BX7
TECTONICPHREATIC
BX2
coarse poor sort
coarse well sort
fine poor sort (dykes)
fine well sort (dykes)
hydrothermal matrix
qz clast qz matrix
ign matrix fine
BXl acid drain back bx BX8 ha cl matrix
BXg phreatomagmatic BX5 ign matrix coarse
BXd diatreme bx
BSs barren silica shoulder pseudo bx coarse qz-al alt
FACIES
alternative
rf rock flour
typicaltohighsulphidation
porphyry/brecciacomplexes
ALTERATION
nul0 trace1 weak2 moderate3 strong4 intense5
PS sub propylitic
ALTERATION FACIES (AFAC)
UA unaltered
PR propylitic
potassicPT
AR argillic
IA intermediate arg
AA - acid sulphate facies
SV silica vuggy
CS clay silica
SM silica massive
vein selvageVNS
ALTERATION STYLE (ASTY)
sed selectSED
adulariaad
ax andalusite
ALT MINERALS (AMIN)
al alunite (udif)
aK K-alunite
clay (udif)cl
di diaspore
do dolomite
dk dickite
pyrophyllitepf
se sericite
qz quartz
sc scapolite
pervasivePER
PAT patchy
FRC fracture
structureSTR
BXM bx matrix
BXC bx clast
clottedCLT
CAV cavities
mordenitemr
an andradite
feldspar (udif)fp
gt garnet (udif)
smectitesm
su specularite
carbonatecb
ch chlorite
halloysiteha
hu heulandite
tourmalineto
vs vesuvianite
corundumco
cx clinopyroxene
cs cristobalite
jarositeja
ka kaolinite
lx lucoxene
zeoliteze
zu zunyite
P2 biotite (2nd PT event)
phyllic:pro-ms ret-sePH
SI silicification
silica aluniteSA
SK skarn
SG silica granular
QT qz-tourmaline
ALT INTENSITY (AINT)
mt magnetite
ep epidote
sd siderite
bi bioite gp gypsum tr tridymite
cz chabazite
il illite
wa wairakite
cd chalcedony
im ilmenite
wo wollastonite
ac actinolite
ca calcite
os opaline silca
ab albite
ms muscovite
na natrolite
SE sericitic (IA)
silica claySC
ICO int contact
px pyroxene
ba barite
ah anhydrite
native SS
aN Na-alunite
ce celadonite
dp diopside
gf graphite
kf k-spar
palygorskitepa
pg phlogopite
ro roscolite
topaztp
zw zinnwaldite
selectSEL REP replacement
phenocrystPHN
matrixMTX
o'printOPN
aplite (ab or kf)AB
CB carbonate
ZE zeolite
SO silica opaline
S1 silica mas vuggy
S2 silica vuggy mas
CA clay alunite
SP silica patchy
SW silica wormy
advanced argAA
PROGRADERETROGRADE
Silica
Group
Alunite
Group
al-ka
Group
kaolin
Group
il-ka
Group
illite
Group
Chlorite
Group
Calc-Silicate
Group
SO
SG
SC CS
AR
SM
SM
PH
se-kf
PH
mica
PT
bi-mt
PT SD
kf-bi-og
SK
cx-gt
SK
tm-qz
Increasing pH
IncreasingTemperature
PT
ac-kf
SK
mt-gt
EPITHERMALDEEPEPITHERMALPORPHYRY
2 3 4 5 6
100
250
300
ALTERATION FACIES AND SUB FACIES - CEG
SJM alteration sub facies overlain on the Corbett & Leach alteration table
PT SK PH PR PS AR AAIA
SA
SV
S2
S1
SP
SW
SG
IA
IA
ch-il
il-sm
AR
ka
sm
CA
AA
pf-al
PH
kf-mica
PR
bi-ep-ac-kf
PR
ch-ep-ca-ad
PS
PH-AA
se
PH
se
CEG ALTERATION FACIES TABLE
(SVM)
(SMV)
qz-ha cl-ha
SG
SH
mm montmorilonite
SY
pr paragonite
la laumonite
rt rutile
conditions of
non-dissociation
retrograde
prograde
Includes the addition of IA to the original Corbett & Leach diagram - codes changed to suit this reference set
tremolitetm
AA
di-dk
epitherm
al
porphyry
transition
anataseaa
BXx collapse breccia
RX recrystallised
HF hornfels
BRECCIA FACIES (BXT)
THE BRECCIA MATRIX COMPONENT NORMALY DEFINES THE BRECCIA FACIES
breccia designator
breccia facies
clast component
clasr rounding (optional)
matrix component
estimate % matrix
phreatic breccias - sourced at depth & drill upwards.
diatreme breccas - originate at surface and drill
downwards. Matrix is clay rich &
hydrothermal fluids
hydrothermal breccias - matrix is sourced from
clasts are sourced form near surface
Matrix is pulverised rock flour &
clasts are sourced from depth
passive process
explosive origin
'BRECCIA RULES OF THUMB'
blockdesignator
RO roscolite (alkalic epi)
CE celadonite (LSE)
MT magnetite (deep PT)
chloritic (IA)CH
Principal Facies Variant Facies
cavity fillCFL structureSTR
VNM vein matrix GMS groundmass BED bedding select
vesicleVES
aH NH-alunite
nc nacrite
nt nontronite
talctc
chalcedonic silSH
SY creamy silica
BXo 'overbank' phreatic breccias - weaker retrograde alt typ / oganic material
alternative
numericnumeric
VBx vein matrix breccia
glassgl
HM heamatite
K2 kspar (2nd PT event)
sodic - calcicSD
og oligoclase
Note: Deep porphyry SODIC-CALCIC (SD) & aplite (AB) inserted - approximate
AB
kf qz ab
SQ sugary quartz (LSE)
DS dark silica (py?)
SQ
4. MINERALISATION 1
boxworkbx
bm microbotriodalbo botryoidal
buck qzBUQ
MINERALISATION TYPE (MTYP)
Oxide Transition
Supergene Enriched
OX TR
SG ENMixed SG/EN/HY
MAS massive
vein undiffVNN
MAB bx mass sx
coatingsCOT
VBX breccia vein
FFL fracture fillling
MINERALISATION STYLE (MSTY)
DSM disseminated
cavity fillingCFL
REP replacement
MTO
CBV carb vein
manto
BVN qz-SX - cp su
SX qz se - cp mo pyCVN
qz-mt +/- SX - cp bnAVN
opaline qzOPQ
SAQ saccharoidal qz
crystalline qzCXQ
chalcedonic qzCHQ
cr crustiform
colloformco
dt dogs tooth
ma massive
oc open cavities gingurogi
QAV qz-adularia vein
MM sweat veinsQMM
HypogeneHY
epithermal vns (undif)EVN
MLV mesothermal vn (undif)
MQV major qz vein
VNR stringer veins
SIV silica veinletts
milky quartz veinsMLQ
rind on clastsRND
MAS massive
BXM bx matrix
bx clastBXC
JAQ jasperoidal qz vein
AMQ amethystine qz vein
DSV dark sx + silica vein
DCV dark sx + clay vein
LSV light sx + clay vein
clear quartzCLQ
no SX
2 process 1 & 2 processes
OX & SX
1 process 1 Process
MX
GSV grey silica vein
Trans OX domTO
OX >> SX
Trans SX domTS
OX << SX
QVN quartz vein
QXV qz-sulphide vein
QCV qz-cb vein
SXV sulphide vein
STK stockwork vns
SHV sheeted veins
WMY wormy silics vns
PORPHYRY
DOMES
LOW SX EP
VEIN TYPES (VTYP)
mt +/- qzMVN
Deep Porphyry Veins
BIV biotite veins
SEV sericite veins
QSV qz-se veins
LQV light qz vein
DQV dark qz vein
QRV qz-ro vein
QLV qz-lm vein
qz-hm veinQHV
ba banded bl bladed
VEINS
WQV white qz vein
Corbett & Leach ALT FACIES TABLE
Silica
Group
Alunite
Group
al-ka
Group
kaolin
Group
il-ka
Group
illite
Group
Chlorite
Group
Calc-Silicate
Group
op
cs
tr
qz
al ha
Silica
op
cs
tr
qz
ha
Silica
ha sm
Silica
Silica
Silica
al ka
Silica
ka
Silica
ka sm
Silica
+ sd
sm
Silica
al
qz
al
ka
qz
ka
qz
qz
conditions of
al
qz
al
ka di
qz+di
al
dk
al
al pf
qz+di
qz+di
dk pf
qz+di
ax
ka sm
qz+sd
ka di
qz+di
ka il sm
qz+sd
sm cb
qz/cz
il sm
dk
qz+sd
cb
qz/cz
il
cb
qz
ka dk
il/il sm
qz+sd
dk
qz+di
pf
dk
se qz
pf
pf
qz+di
pf
qz
se
se
cb
qz
mica/se
ax
pf qz
+ cb
mica qz
se
qz ch
kf
ax al qz
pf qzpf qz
ax al
mica qz
ax mica mica
co qz
kf qz
mica
bi kf
cx mt
bi ac
kf qz
kf cb
cx qz
ca/do
tm qz
ca/doqz + ch
se/mica
Increasing pH
IncreasingTemperature
ac qz
kf ch
ep ac ch qz
kf ca/do
ch qz ep
ad/ab ca/do
gt qz
wo vs
mt
ch il
qz cb
ab/ad
ch cb
qz/cd
il-sm
ch/ch-sm
qz/cd
sm qz/cd
ch-sm/ch
cb
silica
ch-sm/ch
cb/do
silica
ch/ch-sm
zeolite
qz/cd
ch qz/chd
ca do
ad/ab
zeolite
ca/do
ch qz ep
ad/ab
ca/do
zeolite
zeolites
stbhumocznawala
EPITHERMALDEEPEPITHERMALPORPHYRY
PT SK PH AR AA
2 3 4 5 6
100
250
300
HYDROTHERMAL ALTERATION MINERAL SYSTEMS
From: Greg Corbett & Terry Leach, Southwest Pacific Rim Gold Copper Systems - Short Course Manual, 1997
Includes the addition of IA to the original diagram - codes changed to suit this reference set
IA
cb
+ cb
co qz
mica/se
pf qz
non-dissociation
PT SK PH PR PS AR AAIA
dk
qz+di
sugary quartzSGQ
VEIN TEXTURES
ck cockade
cm comb
ms moss
lb lattice bladed
pl plumose
- -
Increasing Temp
100
200
300
al
ja
ha
ka
dk
pf
di
tp, zu
aa
rt
cs
qz
py
ma
sm
il-sm
ch-sm
il
ch
ep
bi
kf, ad
ca
mr
la
wa
IncreasingpH
WEAKLYACIDACIDNEUTRALALKALINE
ORE DEPOSITS
AuAgCuMo
Hedenquist et al ALT TABLE
AdjustedafterHedenquistetal1996fromSocofresourceGeology-ResourceGeologySepcialPublication1,1996
se ?
VNS veins selvage
NWV network vns
NWQ netwk qz vns
NWM netwk mn vns
SulphideSX
vein type
vein familly (porphyries)
gangue minerals (paragenetic order)
vein textures (paragenetic order)
min minerals (paragentic order)
QPV qz-py vein
qz-mn carb veinQMV
GEOCHEMICAL ZONATIONS
ADV adularia vein
SMQ smokey quartz
Myadditionsincludecolours(tempranges),mineralisationbarandse?
bi +/- mt qzBIV
ac +/- mt qzACV
Shallow Porphyry Veins
se-SX qz - mo cp pyDVN
SEV CHV SXVothers
ACV
CHV
SEV
WQV
retrograde
ILP / HLP
ACV ac-SX veins
5. MINERAL RATIOS FOR VECTORING AND MODELLING
ox - no sx cp (only)
cp > bn
0 A
B
C
D
PRINCIPAL COPPER MINERALS
bn
cp
cc
cu
cv
Cu
br
tn
cn
mc
az
ck
cr
pm
bornite
chalcopyrite
chalcocite
cuprite
covellite
native copper
brochantite
tenorite
cubanite
malachite
azurite
chalcantite
chrysocolla
pitch limonite
Cu FeS
CuFeS
Cu S
Cu O
CuS
Cu
Cu (OH) SO
CuO
CuFe S
Cu CO (OH)
Cu (CO ) (OH)
CuSO .5H O
Cu H (Si O )(OH)
5 4
2
2
2
4 6 4
2 3
2 3 2
3 3 2 2
4 2
2 2 2 5 4
57.3%
79.9%
36.0%
79.8%
55.0%
35.0%
63.3%
56.0%
31-34.5%
88.8%
66.4%
23.0%
Cu %
en enargite Cu AsS3 4
100%
OX
TR
SG
HY
py (only)
py > cp
py = cp
py < cp
1
2
3
4
cp < bn
cp = bn
MINERALISATION 3
sol Cu (only) cc (only)
cc > cv
F
sol Cu > py
sol Cu = py
sol Cu < py
G
H
I cc < cv
cc = cv
en (only)
en > py cv > en
cv = en
cv < en
O
P
Q
R
T
U
V
cv (only) S
en < py
en = py
en (only) W
bn (only) E
Cu-Au
PORPHYRY
cv (only)
J
K
L
M
N
ENRICHMENT
BLANKETS
HS
SYSTEMS
py > po
py = po cp > po
cp = po
cp < po
5
6
7
8
W
X
Y
cp (only) V
po (only)
py < po
po (only) Z
PYRRHOTITE
-Cu SKARNS
MINERALISATION 2
antimonysb
at atacamite
MIN MINERALS (MMIN)
ar argentite
as arsenopyrite
chalcopyritecp
ct cuprite
cv covellite
cn cubanite
orpimentor
pl pyrolusite
pm pitch limonite
py pyrite
malachitemc
az azurite
electrumel
en enargite
realgarre
sh scheelite
bismuthinitebt
bn bornite
flouritefl
ga galena
sideritesd
sp sphalerite
cassiteritesn
ct cerussite
ck chalcantite
hessitehs
hz hydrozincite
ja jarosite
native sulphurS
te tellurides
lm limonite
dg digenite
po pyrrhotite
ba barite
fb ferberite
sl selenides
br brochantite
go geothite
st stibnite
ci calverite
hm heamatite
ss sulphosalts
ae anglesite
cc chalcocite
ai alcantite
ma marcasite
tt tennantite
cinnabarnn
molybdenitemo
cr chromite
tenoritetn
Hg mercury
cy chrysocolla
Ag native silver
wd mn wad
ah anhydrite
Cu native copperAu native gold
neotocitene
DS dark sulphides
LS light sulphides
quartzqz
calciteca
carbonatecb
rhodochrositerc gypsumgp
tourmalineto
roscolite micaro
rhodoniterd
magnetitemt
Common vein gangue minerals
magnetitemt
ba barite
ze zeolite
adulariakf rhodochrositerc mn mn wad
so scorodite
lx lucoxene
zc zincite
mn oxidemn
ENRICHMENT
PERIPHERY
CORE
Useful mineral ratios for vectoring purposes
6. 25 °/045°
315°/25° NE
N45W/25NE
BEDDING
E
PUMICE ALIGNMENT
IGNEOUS BANDING
FLOW LINEATION
D/DAZM
W
S
LINEAR FEATURES
315°
N
DIPS
25°
045°
DIP/DIP AZIM
STRIKE/DIP (UK)
STRIKE/DIP (US)
CONTACT (OBSERVED)
DISCONFORMITY
UNCONFROMITY
FOLD AXIS
FOLDS
BOUNDARIES
VEIN
CLEAVAGE
FRACTURE
FOLIATION
FAULT-THRUST
FAULT-REVERSE
FAULT-NORMAL
FAULTS
JOINT
STRUCTURE & EVENTS
PLANNAR FEATURES
BED
LPU
LFL
LIB
UNC
CON
VEN
DIS
FAX
FLN
FTH
FLR
SCL
FOL
SJO
SFR
FAULT (UNDIF) FLT
SCHISTOSITY SCH
BASE PARTIAL OX
BASE SOLUBLE Cu
BASE COMPLETE OX
EVENTS
BCO
BPO
BSO
CONTACT (INFERRED) CIN
MAPPING
CA - ANGLE
COREAXIS
45°
LOGGING
TO CORE
AXIS
STRAIN ELLIPSE
7. =ONE
=acre
MULTIPLIER
4046.856m2
=cubic metre 35.3147 cubic ft
=degree celsius 0.555 ( F-32)
=fathom 1.8288m
=foot 0.3048m
=furlong 201.168m
=gallon 4.54609L
=gallon (US) 3.785412L
=gram 35.273962 x 10 ounces
=gram/tonne 0.0001%
3
= 0.032666oz (troy)/long ton
= 0.02917oz (troy)/short ton
=hectare 10,000m2
= 2.4710538 acres
=inch 25.4mm
=kilogram 2.2046226 pounds
=kilometre 0.621371 miles
=litre 0.219969 gallons
=metre 3.28084 feet
= 1.0936132 yards
=mile 1.609344 km
=mile/hr 0.44704 m/s
=ounce (troy) 31 103477g
=ounce(T)/long ton 30.61224 g/t
=ounce(T)/short ton 34.28571 g/t
=km2 0.386102 miles2
=mile2 640 acres
=acre 2.589988 km2
=stone 6.3502932 kg
=ton, long 1.016047 t (metric)
=ton, short 0.907185 t (metric)
=tonne (t) 0.9842 long tons
=acre 1.1023 short tons
=acre 2204.62 lbs
=yard 0.9144n
CONVERSION FACTORS PERCENTAGES
IGNEOUS ROCKS Phreatic vs Diatreme Breccias