�ݺ�ߣshows by User: ssuser4e111c

�ݺ�ߣshows by User: ssuser4e111c / http://www.slideshare.net/images/logo.gif �ݺ�ߣshows by User: ssuser4e111c / Tue, 20 Jul 2021 08:30:00 GMT �ݺ�ߣShare feed for �ݺ�ߣshows by User: ssuser4e111c Sedimentary Rocks & Field Description of Sedimentary Rocks /slideshow/sedimentary-rocks-field-description-of-sedimentary-rocks/249807268 sedimentrypetroloy-210720083001
Sedimentary Rocks ]]>
Sedimentary Rocks ]]> Tue, 20 Jul 2021 08:30:00 GMT /slideshow/sedimentary-rocks-field-description-of-sedimentary-rocks/249807268 ssuser4e111c@slideshare.net(ssuser4e111c) Sedimentary Rocks & Field Description of Sedimentary Rocks ssuser4e111c Sedimentary Rocks <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/sedimentrypetroloy-210720083001-thumbnail.jpg?width=120&height=120&fit=bounds" /> Sedimentary Rocks

Sedimentary Rocks & Field Description of Sedimentary Rocks from Geology Department | Faculty of Natural Science

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0 Gravity Method | Geophysics | Geology /slideshow/gravity-method-geophysics-geology/249807217 geophysics-210720081617
Definition  Geophysics is the application of method of physics to the study of the earth.  On the other sense, it is a subject of natural science concerned with the physical processes and the physical properties of the earth and its surrounding space environment and the use of co-ordinate methods for the analysis.  It involves the application of physical theories and measurements to discover the properties and processes of the earth.]]>
Definition  Geophysics is the application of method of physics to the study of the earth.  On the other sense, it is a subject of natural science concerned with the physical processes and the physical properties of the earth and its surrounding space environment and the use of co-ordinate methods for the analysis.  It involves the application of physical theories and measurements to discover the properties and processes of the earth.]]> Tue, 20 Jul 2021 08:16:17 GMT /slideshow/gravity-method-geophysics-geology/249807217 ssuser4e111c@slideshare.net(ssuser4e111c) Gravity Method | Geophysics | Geology ssuser4e111c Definition  Geophysics is the application of method of physics to the study of the earth.  On the other sense, it is a subject of natural science concerned with the physical processes and the physical properties of the earth and its surrounding space environment and the use of co-ordinate methods for the analysis.  It involves the application of physical theories and measurements to discover the properties and processes of the earth. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/geophysics-210720081617-thumbnail.jpg?width=120&height=120&fit=bounds" /> Definition  Geophysics is the application of method of physics to the study of the earth.  On the other sense, it is a subject of natural science concerned with the physical processes and the physical properties of the earth and its surrounding space environment and the use of co-ordinate methods for the analysis.  It involves the application of physical theories and measurements to discover the properties and processes of the earth.

Gravity Method | Geophysics | Geology from Geology Department | Faculty of Natural Science

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0 Groundwater aquifers /ssuser4e111c/groundwater-aquifers groundwaterpdf-210720073438
Ground Water aquifers ]]>
Ground Water aquifers ]]> Tue, 20 Jul 2021 07:34:37 GMT /ssuser4e111c/groundwater-aquifers ssuser4e111c@slideshare.net(ssuser4e111c) Groundwater aquifers ssuser4e111c Ground Water aquifers <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/groundwaterpdf-210720073438-thumbnail.jpg?width=120&height=120&fit=bounds" /> Ground Water aquifers

Groundwater aquifers from Geology Department | Faculty of Natural Science

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0 SALT RANGE | GEOLOGY OF PAKISTAN /slideshow/salt-range-geology-of-pakistan/249803761 geologypdf-210719122547
INTRODUCTION The Indus Basin of Pakistan is divided into two parts i.e. 3 Lower Indus Basin and Upper Indus Basin. The Upper Indus Basin is further divided by Sargodha high way into two parts. Towards the east of the Sargodha highway in Potwar Plateau and towards the west is Kohat Plateau. The region of the North Punjab called as Potwar Plateau is bound in the South by Salt range and in North by MBT as shown below.]]>
INTRODUCTION The Indus Basin of Pakistan is divided into two parts i.e. 3 Lower Indus Basin and Upper Indus Basin. The Upper Indus Basin is further divided by Sargodha high way into two parts. Towards the east of the Sargodha highway in Potwar Plateau and towards the west is Kohat Plateau. The region of the North Punjab called as Potwar Plateau is bound in the South by Salt range and in North by MBT as shown below.]]> Mon, 19 Jul 2021 12:25:47 GMT /slideshow/salt-range-geology-of-pakistan/249803761 ssuser4e111c@slideshare.net(ssuser4e111c) SALT RANGE | GEOLOGY OF PAKISTAN ssuser4e111c INTRODUCTION The Indus Basin of Pakistan is divided into two parts i.e. 3 Lower Indus Basin and Upper Indus Basin. The Upper Indus Basin is further divided by Sargodha high way into two parts. Towards the east of the Sargodha highway in Potwar Plateau and towards the west is Kohat Plateau. The region of the North Punjab called as Potwar Plateau is bound in the South by Salt range and in North by MBT as shown below. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/geologypdf-210719122547-thumbnail.jpg?width=120&height=120&fit=bounds" /> INTRODUCTION The Indus Basin of Pakistan is divided into two parts i.e. 3 Lower Indus Basin and Upper Indus Basin. The Upper Indus Basin is further divided by Sargodha high way into two parts. Towards the east of the Sargodha highway in Potwar Plateau and towards the west is Kohat Plateau. The region of the North Punjab called as Potwar Plateau is bound in the South by Salt range and in North by MBT as shown below.

SALT RANGE | GEOLOGY OF PAKISTAN from Geology Department | Faculty of Natural Science

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0 Classification of Ore Deposits | Economic Geology /slideshow/classification-of-ore-deposits-economic-geology/249803625 assignment-210719115513
CLASSIFICATION OF ORE DEPOSITS The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore deposits are generally found enclosed within the country rocks. The ore deposits are formed in many different ways. Depending upon the process that may operate to produce them, the ore deposits may be classified as follow:  Magmatic ore deposits.  Sublimation ore deposits.  Pegmatitic ore deposits.  Contact metasomatic ore deposits.  Hydrothermal ore deposits  Cavity filling deposits.  Replacement deposits.  Sedimentation ore deposits.  Evaporation ore deposits.  Residual and mechanical concentration deposits  Metamorphic ore deposits. MAGMATIC ORE DEPOSITS: The magmatic ore deposits are the magmatic products which crystallize from magmas. The magmatic ore deposits are classified as follows: o Early magmatic deposits o Late magmatic deposits Early magmatic deposits: Early magmatic deposits are formed during the early stage of the magmatic period. In this case the ore minerals crystallize earlier than the rock silicates. The Minerals of Nickel, Chromium, and Platinum are usually found as early magmatic deposits. The early magmatic deposits can be sub divided into two groups: o Dissemination deposits o Segregation deposits Dissemination deposits: When magma crystallizes conditions, a granular igneous rock is formed. In such a rock early formed crystals of may occur in dissemination. Segregation deposits: Magmatic segregation deposits are formed as a result of gravitative crystallization differentiation. In case, the ore mineral which crystallize early, get ocean-trated on a particular part of igneous part. The ore deposits thus formed are known as “Segregation deposits”. rly under seated ore minerals such Late Magmatic Deposits: The ore deposits which are formed to called late magmatic deposits. The late magmatic deposits contain those ore minerals which have crystallized at rather low temperature from the residual magma. The magma which is left after crystallization of early for is called residual magma. This magma frequently contains many ore minerals. The late magmatic deposits include most of the magmatic deposits of iron and titanium ores, these deposits are almost always associated with mafic igneous rocks. SUBLIMATION DEPOSITS: Sublimation is a very minor process of formation of ore deposits. Sublimation deposits contain only those minerals which have been volatilized by hear and subsequently redeposit in the same form at low temperature and pressure. The sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur of this origin has been mined in Japan, Italy, and Mexico. ]]>
CLASSIFICATION OF ORE DEPOSITS The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore deposits are generally found enclosed within the country rocks. The ore deposits are formed in many different ways. Depending upon the process that may operate to produce them, the ore deposits may be classified as follow:  Magmatic ore deposits.  Sublimation ore deposits.  Pegmatitic ore deposits.  Contact metasomatic ore deposits.  Hydrothermal ore deposits  Cavity filling deposits.  Replacement deposits.  Sedimentation ore deposits.  Evaporation ore deposits.  Residual and mechanical concentration deposits  Metamorphic ore deposits. MAGMATIC ORE DEPOSITS: The magmatic ore deposits are the magmatic products which crystallize from magmas. The magmatic ore deposits are classified as follows: o Early magmatic deposits o Late magmatic deposits Early magmatic deposits: Early magmatic deposits are formed during the early stage of the magmatic period. In this case the ore minerals crystallize earlier than the rock silicates. The Minerals of Nickel, Chromium, and Platinum are usually found as early magmatic deposits. The early magmatic deposits can be sub divided into two groups: o Dissemination deposits o Segregation deposits Dissemination deposits: When magma crystallizes conditions, a granular igneous rock is formed. In such a rock early formed crystals of may occur in dissemination. Segregation deposits: Magmatic segregation deposits are formed as a result of gravitative crystallization differentiation. In case, the ore mineral which crystallize early, get ocean-trated on a particular part of igneous part. The ore deposits thus formed are known as “Segregation deposits”. rly under seated ore minerals such Late Magmatic Deposits: The ore deposits which are formed to called late magmatic deposits. The late magmatic deposits contain those ore minerals which have crystallized at rather low temperature from the residual magma. The magma which is left after crystallization of early for is called residual magma. This magma frequently contains many ore minerals. The late magmatic deposits include most of the magmatic deposits of iron and titanium ores, these deposits are almost always associated with mafic igneous rocks. SUBLIMATION DEPOSITS: Sublimation is a very minor process of formation of ore deposits. Sublimation deposits contain only those minerals which have been volatilized by hear and subsequently redeposit in the same form at low temperature and pressure. The sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur of this origin has been mined in Japan, Italy, and Mexico. ]]> Mon, 19 Jul 2021 11:55:13 GMT /slideshow/classification-of-ore-deposits-economic-geology/249803625 ssuser4e111c@slideshare.net(ssuser4e111c) Classification of Ore Deposits | Economic Geology ssuser4e111c CLASSIFICATION OF ORE DEPOSITS The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore deposits are generally found enclosed within the country rocks. The ore deposits are formed in many different ways. Depending upon the process that may operate to produce them, the ore deposits may be classified as follow:  Magmatic ore deposits.  Sublimation ore deposits.  Pegmatitic ore deposits.  Contact metasomatic ore deposits.  Hydrothermal ore deposits  Cavity filling deposits.  Replacement deposits.  Sedimentation ore deposits.  Evaporation ore deposits.  Residual and mechanical concentration deposits  Metamorphic ore deposits. MAGMATIC ORE DEPOSITS: The magmatic ore deposits are the magmatic products which crystallize from magmas. The magmatic ore deposits are classified as follows: o Early magmatic deposits o Late magmatic deposits Early magmatic deposits: Early magmatic deposits are formed during the early stage of the magmatic period. In this case the ore minerals crystallize earlier than the rock silicates. The Minerals of Nickel, Chromium, and Platinum are usually found as early magmatic deposits. The early magmatic deposits can be sub divided into two groups: o Dissemination deposits o Segregation deposits Dissemination deposits: When magma crystallizes conditions, a granular igneous rock is formed. In such a rock early formed crystals of may occur in dissemination. Segregation deposits: Magmatic segregation deposits are formed as a result of gravitative crystallization differentiation. In case, the ore mineral which crystallize early, get ocean-trated on a particular part of igneous part. The ore deposits thus formed are known as “Segregation deposits”. rly under seated ore minerals such Late Magmatic Deposits: The ore deposits which are formed to called late magmatic deposits. The late magmatic deposits contain those ore minerals which have crystallized at rather low temperature from the residual magma. The magma which is left after crystallization of early for is called residual magma. This magma frequently contains many ore minerals. The late magmatic deposits include most of the magmatic deposits of iron and titanium ores, these deposits are almost always associated with mafic igneous rocks. SUBLIMATION DEPOSITS: Sublimation is a very minor process of formation of ore deposits. Sublimation deposits contain only those minerals which have been volatilized by hear and subsequently redeposit in the same form at low temperature and pressure. The sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur of this origin has been mined in Japan, Italy, and Mexico. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/assignment-210719115513-thumbnail.jpg?width=120&height=120&fit=bounds" /> CLASSIFICATION OF ORE DEPOSITS The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore deposits are generally found enclosed within the country rocks. The ore deposits are formed in many different ways. Depending upon the process that may operate to produce them, the ore deposits may be classified as follow:  Magmatic ore deposits.  Sublimation ore deposits.  Pegmatitic ore deposits.  Contact metasomatic ore deposits.  Hydrothermal ore deposits  Cavity filling deposits.  Replacement deposits.  Sedimentation ore deposits.  Evaporation ore deposits.  Residual and mechanical concentration deposits  Metamorphic ore deposits. MAGMATIC ORE DEPOSITS: The magmatic ore deposits are the magmatic products which crystallize from magmas. The magmatic ore deposits are classified as follows: o Early magmatic deposits o Late magmatic deposits Early magmatic deposits: Early magmatic deposits are formed during the early stage of the magmatic period. In this case the ore minerals crystallize earlier than the rock silicates. The Minerals of Nickel, Chromium, and Platinum are usually found as early magmatic deposits. The early magmatic deposits can be sub divided into two groups: o Dissemination deposits o Segregation deposits Dissemination deposits: When magma crystallizes conditions, a granular igneous rock is formed. In such a rock early formed crystals of may occur in dissemination. Segregation deposits: Magmatic segregation deposits are formed as a result of gravitative crystallization differentiation. In case, the ore mineral which crystallize early, get ocean-trated on a particular part of igneous part. The ore deposits thus formed are known as “Segregation deposits”. rly under seated ore minerals such Late Magmatic Deposits: The ore deposits which are formed to called late magmatic deposits. The late magmatic deposits contain those ore minerals which have crystallized at rather low temperature from the residual magma. The magma which is left after crystallization of early for is called residual magma. This magma frequently contains many ore minerals. The late magmatic deposits include most of the magmatic deposits of iron and titanium ores, these deposits are almost always associated with mafic igneous rocks. SUBLIMATION DEPOSITS: Sublimation is a very minor process of formation of ore deposits. Sublimation deposits contain only those minerals which have been volatilized by hear and subsequently redeposit in the same form at low temperature and pressure. The sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur of this origin has been mined in Japan, Italy, and Mexico.

Classification of Ore Deposits | Economic Geology from Geology Department | Faculty of Natural Science

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0 Basics of GIS | Base Map | Georeferencing | Satellite Imagery | Step by Step /ssuser4e111c/basics-of-gis-base-map-georeferencing-satellite-imagery gisassignment-210719113246
Introduction GIS Stands for - Geographic Information System G + IS (Geography) + (Information System) Geography is the science that Studies the land feature, inhabitants, and the phenomena of Earth. Information system – A way of manipulating the information digitally (Using computer or digital Device).]]>
Introduction GIS Stands for - Geographic Information System G + IS (Geography) + (Information System) Geography is the science that Studies the land feature, inhabitants, and the phenomena of Earth. Information system – A way of manipulating the information digitally (Using computer or digital Device).]]> Mon, 19 Jul 2021 11:32:45 GMT /ssuser4e111c/basics-of-gis-base-map-georeferencing-satellite-imagery ssuser4e111c@slideshare.net(ssuser4e111c) Basics of GIS | Base Map | Georeferencing | Satellite Imagery | Step by Step ssuser4e111c Introduction GIS Stands for - Geographic Information System G + IS (Geography) + (Information System) Geography is the science that Studies the land feature, inhabitants, and the phenomena of Earth. Information system – A way of manipulating the information digitally (Using computer or digital Device). <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/gisassignment-210719113246-thumbnail.jpg?width=120&height=120&fit=bounds" /> Introduction GIS Stands for - Geographic Information System G + IS (Geography) + (Information System) Geography is the science that Studies the land feature, inhabitants, and the phenomena of Earth. Information system – A way of manipulating the information digitally (Using computer or digital Device).

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0 https://cdn.slidesharecdn.com/profile-photo-ssuser4e111c-48x48.jpg?cb=1626696636 https://cdn.slidesharecdn.com/ss_thumbnails/sedimentrypetroloy-210720083001-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/sedimentary-rocks-field-description-of-sedimentary-rocks/249807268 Sedimentary Rocks & Fi... https://cdn.slidesharecdn.com/ss_thumbnails/geophysics-210720081617-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/gravity-method-geophysics-geology/249807217 Gravity Method | Geoph... https://cdn.slidesharecdn.com/ss_thumbnails/groundwaterpdf-210720073438-thumbnail.jpg?width=320&height=320&fit=bounds ssuser4e111c/groundwater-aquifers Groundwater aquifers