ºÝºÝߣshows by User: kyikyaw2 / http://www.slideshare.net/images/logo.gif ºÝºÝߣshows by User: kyikyaw2 / Sun, 21 Jan 2018 04:02:55 GMT ºÝºÝߣShare feed for ºÝºÝߣshows by User: kyikyaw2 Arakan coastal ranges, kyi khin & and khin zaw, 2017.pptx /slideshow/arakan-coastal-ranges-kyi-khin-and-khin-zaw-2017pptx/86464121 arakancoastalrangeskkkz2017-180121040255
The Bengal-Arakan Neogene basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since late Cenozoic (Kyi Khin et al., 2014, 2017). The basin occupies the eastern part of Paleo-Bengal basin, the biggest basin of the world in Cenozoic. It is located at the unique tectonic setting; a juncture of the collision zone between the Indian and Asian continents to the north and the subduction zone between the Indian Plate and Myanmar Plate to the east. The purpose of the study is to shed some light on the sedimentation in the distal foreland basin of the Himalaya-Bengal System, related with control on timing and distribution of erosional fluxes derived from the uplifted Himalayas since Early Miocene. Chemical weathering strongly affects the major-element geochemistry and mineralogy of siliciclastic sediments. The predicted weathering trend line intersects the feldspar and shows the proportion of plagioclase and K-feldspar of the fresh rock between granodiorite and granite composition. The presentation will focus on the results of integrated study of sequence stratigraphy on the Miocene sediments and the provenance studies based on the petrography and chemical composition of sandstones and shales in order to interpret the weathering episode and relationship between tectonic denudation of Himalaya orogenic belts and reciprocal sedimentation related with foreland thrusting of Himalaya-Bengal System.]]>
The Bengal-Arakan Neogene basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since late Cenozoic (Kyi Khin et al., 2014, 2017). The basin occupies the eastern part of Paleo-Bengal basin, the biggest basin of the world in Cenozoic. It is located at the unique tectonic setting; a juncture of the collision zone between the Indian and Asian continents to the north and the subduction zone between the Indian Plate and Myanmar Plate to the east. The purpose of the study is to shed some light on the sedimentation in the distal foreland basin of the Himalaya-Bengal System, related with control on timing and distribution of erosional fluxes derived from the uplifted Himalayas since Early Miocene. Chemical weathering strongly affects the major-element geochemistry and mineralogy of siliciclastic sediments. The predicted weathering trend line intersects the feldspar and shows the proportion of plagioclase and K-feldspar of the fresh rock between granodiorite and granite composition. The presentation will focus on the results of integrated study of sequence stratigraphy on the Miocene sediments and the provenance studies based on the petrography and chemical composition of sandstones and shales in order to interpret the weathering episode and relationship between tectonic denudation of Himalaya orogenic belts and reciprocal sedimentation related with foreland thrusting of Himalaya-Bengal System.]]> Sun, 21 Jan 2018 04:02:55 GMT /slideshow/arakan-coastal-ranges-kyi-khin-and-khin-zaw-2017pptx/86464121 kyikyaw2@slideshare.net(kyikyaw2) Arakan coastal ranges, kyi khin & and khin zaw, 2017.pptx kyikyaw2 The Bengal-Arakan Neogene basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since late Cenozoic (Kyi Khin et al., 2014, 2017). The basin occupies the eastern part of Paleo-Bengal basin, the biggest basin of the world in Cenozoic. It is located at the unique tectonic setting; a juncture of the collision zone between the Indian and Asian continents to the north and the subduction zone between the Indian Plate and Myanmar Plate to the east. The purpose of the study is to shed some light on the sedimentation in the distal foreland basin of the Himalaya-Bengal System, related with control on timing and distribution of erosional fluxes derived from the uplifted Himalayas since Early Miocene. Chemical weathering strongly affects the major-element geochemistry and mineralogy of siliciclastic sediments. The predicted weathering trend line intersects the feldspar and shows the proportion of plagioclase and K-feldspar of the fresh rock between granodiorite and granite composition. The presentation will focus on the results of integrated study of sequence stratigraphy on the Miocene sediments and the provenance studies based on the petrography and chemical composition of sandstones and shales in order to interpret the weathering episode and relationship between tectonic denudation of Himalaya orogenic belts and reciprocal sedimentation related with foreland thrusting of Himalaya-Bengal System. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/arakancoastalrangeskkkz2017-180121040255-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The Bengal-Arakan Neogene basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since late Cenozoic (Kyi Khin et al., 2014, 2017). The basin occupies the eastern part of Paleo-Bengal basin, the biggest basin of the world in Cenozoic. It is located at the unique tectonic setting; a juncture of the collision zone between the Indian and Asian continents to the north and the subduction zone between the Indian Plate and Myanmar Plate to the east. The purpose of the study is to shed some light on the sedimentation in the distal foreland basin of the Himalaya-Bengal System, related with control on timing and distribution of erosional fluxes derived from the uplifted Himalayas since Early Miocene. Chemical weathering strongly affects the major-element geochemistry and mineralogy of siliciclastic sediments. The predicted weathering trend line intersects the feldspar and shows the proportion of plagioclase and K-feldspar of the fresh rock between granodiorite and granite composition. The presentation will focus on the results of integrated study of sequence stratigraphy on the Miocene sediments and the provenance studies based on the petrography and chemical composition of sandstones and shales in order to interpret the weathering episode and relationship between tectonic denudation of Himalaya orogenic belts and reciprocal sedimentation related with foreland thrusting of Himalaya-Bengal System.
Arakan coastal ranges, kyi khin & and khin zaw, 2017.pptx from KYI KHIN
]]> 512 7 https://cdn.slidesharecdn.com/ss_thumbnails/arakancoastalrangeskkkz2017-180121040255-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Role of Geologists in Natural Hazard Mapping and Application_Dr Kyi Khin_MGSS 21st Annual Memorial Maganine 2016 /slideshow/role-of-geologists-in-natural-hazard-mapping-and-applicationdr-kyi-khinmgss-21st-annual-memorial-maganine-2016-68738347/68738347 a9648d70-47cd-4e05-90b1-f3730b4b43c9-161112031734
Every year, natural hazard events threaten lives and livelihoods, resulting in deaths and billions of dollars in damage. Many geoscientists and various institutions are working with many partners to monitor, assess, and conduct targeted research on a wide range of natural hazards so that policymakers and the public have the understanding to enhance preparedness, response and resilience. For planning and risk assessment to tackle the Natural Hazards for public awareness, alarming and evacuation, Hazard Maps are essentially needed for institutions and governmental working committees of Natural Disaster Prevention, in future. ]]>
Every year, natural hazard events threaten lives and livelihoods, resulting in deaths and billions of dollars in damage. Many geoscientists and various institutions are working with many partners to monitor, assess, and conduct targeted research on a wide range of natural hazards so that policymakers and the public have the understanding to enhance preparedness, response and resilience. For planning and risk assessment to tackle the Natural Hazards for public awareness, alarming and evacuation, Hazard Maps are essentially needed for institutions and governmental working committees of Natural Disaster Prevention, in future. ]]> Sat, 12 Nov 2016 03:17:34 GMT /slideshow/role-of-geologists-in-natural-hazard-mapping-and-applicationdr-kyi-khinmgss-21st-annual-memorial-maganine-2016-68738347/68738347 kyikyaw2@slideshare.net(kyikyaw2) Role of Geologists in Natural Hazard Mapping and Application_Dr Kyi Khin_MGSS 21st Annual Memorial Maganine 2016 kyikyaw2 Every year, natural hazard events threaten lives and livelihoods, resulting in deaths and billions of dollars in damage. Many geoscientists and various institutions are working with many partners to monitor, assess, and conduct targeted research on a wide range of natural hazards so that policymakers and the public have the understanding to enhance preparedness, response and resilience. For planning and risk assessment to tackle the Natural Hazards for public awareness, alarming and evacuation, Hazard Maps are essentially needed for institutions and governmental working committees of Natural Disaster Prevention, in future. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/a9648d70-47cd-4e05-90b1-f3730b4b43c9-161112031734-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Every year, natural hazard events threaten lives and livelihoods, resulting in deaths and billions of dollars in damage. Many geoscientists and various institutions are working with many partners to monitor, assess, and conduct targeted research on a wide range of natural hazards so that policymakers and the public have the understanding to enhance preparedness, response and resilience. For planning and risk assessment to tackle the Natural Hazards for public awareness, alarming and evacuation, Hazard Maps are essentially needed for institutions and governmental working committees of Natural Disaster Prevention, in future.
Role of Geologists in Natural Hazard Mapping and Application_Dr Kyi Khin_MGSS 21st Annual Memorial Maganine 2016 from KYI KHIN
]]> 1234 6 https://cdn.slidesharecdn.com/ss_thumbnails/a9648d70-47cd-4e05-90b1-f3730b4b43c9-161112031734-thumbnail.jpg?width=120&height=120&fit=bounds document White http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Outcrops of SG_KK & KL_August 2016_Final_20.09.16 /slideshow/outcrops-of-sgkk-klaugust-2016final200916/66236611 c871341a-2ccc-4fcc-910d-ba1c11f7d217-160921003012
This compilation was aimed to record for rare geological outcrops which were gradually diminished by infrastructural and construction projects. Sharing information among fellow geologists working in Singapore and abroad. ]]>
This compilation was aimed to record for rare geological outcrops which were gradually diminished by infrastructural and construction projects. Sharing information among fellow geologists working in Singapore and abroad. ]]> Wed, 21 Sep 2016 00:30:11 GMT /slideshow/outcrops-of-sgkk-klaugust-2016final200916/66236611 kyikyaw2@slideshare.net(kyikyaw2) Outcrops of SG_KK & KL_August 2016_Final_20.09.16 kyikyaw2 This compilation was aimed to record for rare geological outcrops which were gradually diminished by infrastructural and construction projects. Sharing information among fellow geologists working in Singapore and abroad. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/c871341a-2ccc-4fcc-910d-ba1c11f7d217-160921003012-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> This compilation was aimed to record for rare geological outcrops which were gradually diminished by infrastructural and construction projects. Sharing information among fellow geologists working in Singapore and abroad.
Outcrops of SG_KK & KL_August 2016_Final_20.09.16 from KYI KHIN
]]> 1845 4 https://cdn.slidesharecdn.com/ss_thumbnails/c871341a-2ccc-4fcc-910d-ba1c11f7d217-160921003012-thumbnail.jpg?width=120&height=120&fit=bounds presentation White http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Bed Rock ºÝºÝߣs in Shimanto Belt_Kyi Khin & Fukuda, 2001, 17th Applied geological Society , Kyushu Branch, japan /slideshow/bed-rock-slides-in-shimanto-beltkyi-khin-fukuda-2001-17th-applied-geological-society-kyushu-branch-japan/63863311 051eb3c3-e1e8-414a-af53-eb2ee5c4527c-160709064403
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]]> Sat, 09 Jul 2016 06:44:03 GMT /slideshow/bed-rock-slides-in-shimanto-beltkyi-khin-fukuda-2001-17th-applied-geological-society-kyushu-branch-japan/63863311 kyikyaw2@slideshare.net(kyikyaw2) Bed Rock ºÝºÝߣs in Shimanto Belt_Kyi Khin & Fukuda, 2001, 17th Applied geological Society , Kyushu Branch, japan kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/051eb3c3-e1e8-414a-af53-eb2ee5c4527c-160709064403-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
Bed Rock ºÝºÝߣs in Shimanto Belt_Kyi Khin & Fukuda, 2001, 17th Applied geological Society , Kyushu Branch, japan from KYI KHIN
]]> 111 4 https://cdn.slidesharecdn.com/ss_thumbnails/051eb3c3-e1e8-414a-af53-eb2ee5c4527c-160709064403-thumbnail.jpg?width=120&height=120&fit=bounds document 000000 http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 OIL SEEPAGES TRAPPED IN MIOCENE FORCED REGRESSIVE SILICICLASTIC /slideshow/oil-seepages-trapped-in-miocene-forced-regressive-siliciclastic/58354730 84c4bff2-73c0-4539-a413-c71121d2e4d6-160217033139
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]]> Wed, 17 Feb 2016 03:31:39 GMT /slideshow/oil-seepages-trapped-in-miocene-forced-regressive-siliciclastic/58354730 kyikyaw2@slideshare.net(kyikyaw2) OIL SEEPAGES TRAPPED IN MIOCENE FORCED REGRESSIVE SILICICLASTIC kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/84c4bff2-73c0-4539-a413-c71121d2e4d6-160217033139-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
OIL SEEPAGES TRAPPED IN MIOCENE FORCED REGRESSIVE SILICICLASTIC from KYI KHIN
]]> 480 6 https://cdn.slidesharecdn.com/ss_thumbnails/84c4bff2-73c0-4539-a413-c71121d2e4d6-160217033139-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 GEOTECHNICAL INVESTIGATIONS /slideshow/geotechnical-investigations-57816622/57816622 bf2e7a40-234c-4c8e-b6b9-7d057ef95deb-160203072856
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]]> Wed, 03 Feb 2016 07:28:56 GMT /slideshow/geotechnical-investigations-57816622/57816622 kyikyaw2@slideshare.net(kyikyaw2) GEOTECHNICAL INVESTIGATIONS kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/bf2e7a40-234c-4c8e-b6b9-7d057ef95deb-160203072856-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
GEOTECHNICAL INVESTIGATIONS from KYI KHIN
]]> 3667 7 https://cdn.slidesharecdn.com/ss_thumbnails/bf2e7a40-234c-4c8e-b6b9-7d057ef95deb-160203072856-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Some Microscopic features of Volcaniclastic Rocks in Jurong Formation, Singapore /slideshow/some-microscopic-features-of-volcaniclastic-rocks-in-jurong-formation-singapore/55809086 0272f670-e7d5-4a94-a43e-662bfaf6a4e1-151204063555-lva1-app6891
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]]> Fri, 04 Dec 2015 06:35:55 GMT /slideshow/some-microscopic-features-of-volcaniclastic-rocks-in-jurong-formation-singapore/55809086 kyikyaw2@slideshare.net(kyikyaw2) Some Microscopic features of Volcaniclastic Rocks in Jurong Formation, Singapore kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/0272f670-e7d5-4a94-a43e-662bfaf6a4e1-151204063555-lva1-app6891-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
Some Microscopic features of Volcaniclastic Rocks in Jurong Formation, Singapore from KYI KHIN
]]> 776 6 https://cdn.slidesharecdn.com/ss_thumbnails/0272f670-e7d5-4a94-a43e-662bfaf6a4e1-151204063555-lva1-app6891-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Revisit to Baronga Islands, KyiKhin & AungMoe, 2015 (Rev. 3) /slideshow/revisit-to-baronga-islands-kk-am-2015-r3/55068244 d88d1480-079f-48a7-99e2-1b82a20957dc-151113064049-lva1-app6891
Presentation on Structural analysis of Slump Folds from Neogene Deep-marine Slope - Shallow Marine Deposits to get some trace of India-Asia subduction and Collision.]]>
Presentation on Structural analysis of Slump Folds from Neogene Deep-marine Slope - Shallow Marine Deposits to get some trace of India-Asia subduction and Collision.]]> Fri, 13 Nov 2015 06:40:49 GMT /slideshow/revisit-to-baronga-islands-kk-am-2015-r3/55068244 kyikyaw2@slideshare.net(kyikyaw2) Revisit to Baronga Islands, KyiKhin & AungMoe, 2015 (Rev. 3) kyikyaw2 Presentation on Structural analysis of Slump Folds from Neogene Deep-marine Slope - Shallow Marine Deposits to get some trace of India-Asia subduction and Collision. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/d88d1480-079f-48a7-99e2-1b82a20957dc-151113064049-lva1-app6891-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation on Structural analysis of Slump Folds from Neogene Deep-marine Slope - Shallow Marine Deposits to get some trace of India-Asia subduction and Collision.
Revisit to Baronga Islands, KyiKhin & AungMoe, 2015 (Rev. 3) from KYI KHIN
]]> 445 4 https://cdn.slidesharecdn.com/ss_thumbnails/d88d1480-079f-48a7-99e2-1b82a20957dc-151113064049-lva1-app6891-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 LANDSLIDES /slideshow/landslides-52417555/52417555 fd2f4ad5-3d23-4814-85c5-80d52c739c7d-150904105402-lva1-app6892
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]]> Fri, 04 Sep 2015 10:54:02 GMT /slideshow/landslides-52417555/52417555 kyikyaw2@slideshare.net(kyikyaw2) LANDSLIDES kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/fd2f4ad5-3d23-4814-85c5-80d52c739c7d-150904105402-lva1-app6892-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
LANDSLIDES from KYI KHIN
]]> 4156 16 https://cdn.slidesharecdn.com/ss_thumbnails/fd2f4ad5-3d23-4814-85c5-80d52c739c7d-150904105402-lva1-app6892-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Understanding the sedimentary rocks - Geotalk 2 (MGSS) /kyikyaw2/understanding-the-sedimentary-rocks-geotalk-2-mgss dc17d322-54b3-46f4-a3e8-aaf66b1f9cd5-150807025611-lva1-app6891
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]]> Fri, 07 Aug 2015 02:56:11 GMT /kyikyaw2/understanding-the-sedimentary-rocks-geotalk-2-mgss kyikyaw2@slideshare.net(kyikyaw2) Understanding the sedimentary rocks - Geotalk 2 (MGSS) kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/dc17d322-54b3-46f4-a3e8-aaf66b1f9cd5-150807025611-lva1-app6891-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
Understanding the sedimentary rocks - Geotalk 2 (MGSS) from KYI KHIN
]]> 8052 9 https://cdn.slidesharecdn.com/ss_thumbnails/dc17d322-54b3-46f4-a3e8-aaf66b1f9cd5-150807025611-lva1-app6891-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Geotectonic setting of Singapore and SE Asia /kyikyaw2/geotectonic-setting-of-singapore-and-se-asia geotectonicsettingofsingaporeandseasia-141209030216-conversion-gate01
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]]> Tue, 09 Dec 2014 03:02:16 GMT /kyikyaw2/geotectonic-setting-of-singapore-and-se-asia kyikyaw2@slideshare.net(kyikyaw2) Geotectonic setting of Singapore and SE Asia kyikyaw2 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/geotectonicsettingofsingaporeandseasia-141209030216-conversion-gate01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br>
Geotectonic setting of Singapore and SE Asia from KYI KHIN
]]> 2226 5 https://cdn.slidesharecdn.com/ss_thumbnails/geotectonicsettingofsingaporeandseasia-141209030216-conversion-gate01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Neogene sedimentary fringe (2012) /slideshow/neogene-sedimentary-fringe-2012/41608883 neogenesedimentaryfringeaapg2012-141116002032-conversion-gate02
Presentation at ICE, Singapore by AAPG, 2012]]>
Presentation at ICE, Singapore by AAPG, 2012]]> Sun, 16 Nov 2014 00:20:32 GMT /slideshow/neogene-sedimentary-fringe-2012/41608883 kyikyaw2@slideshare.net(kyikyaw2) Neogene sedimentary fringe (2012) kyikyaw2 Presentation at ICE, Singapore by AAPG, 2012 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/neogenesedimentaryfringeaapg2012-141116002032-conversion-gate02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation at ICE, Singapore by AAPG, 2012
Neogene sedimentary fringe (2012) from KYI KHIN
]]> 786 2 https://cdn.slidesharecdn.com/ss_thumbnails/neogenesedimentaryfringeaapg2012-141116002032-conversion-gate02-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Core orientation in drilling of ROCKS for Site Investigation Works /slideshow/core-orientation-in-drilling-of-rocks/41608607 coreorientationindrilling-141116000029-conversion-gate01
Presentation on Underground Space Technology]]>
Presentation on Underground Space Technology]]> Sun, 16 Nov 2014 00:00:28 GMT /slideshow/core-orientation-in-drilling-of-rocks/41608607 kyikyaw2@slideshare.net(kyikyaw2) Core orientation in drilling of ROCKS for Site Investigation Works kyikyaw2 Presentation on Underground Space Technology <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/coreorientationindrilling-141116000029-conversion-gate01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation on Underground Space Technology
Core orientation in drilling of ROCKS for Site Investigation Works from KYI KHIN
]]> 5661 8 https://cdn.slidesharecdn.com/ss_thumbnails/coreorientationindrilling-141116000029-conversion-gate01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Arbura formation (forced regressive sequences) kyushu, japan 2005 /slideshow/arbura-formation-forced-regressive-sequences-kyushu-japan-2005-41608557/41608557 arburaformationforcedregressivesequenceskyushujapan2005-141115235656-conversion-gate02
Sequence Stratigraphic Study in Myazaki Group]]>
Sequence Stratigraphic Study in Myazaki Group]]> Sat, 15 Nov 2014 23:56:56 GMT /slideshow/arbura-formation-forced-regressive-sequences-kyushu-japan-2005-41608557/41608557 kyikyaw2@slideshare.net(kyikyaw2) Arbura formation (forced regressive sequences) kyushu, japan 2005 kyikyaw2 Sequence Stratigraphic Study in Myazaki Group <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/arburaformationforcedregressivesequenceskyushujapan2005-141115235656-conversion-gate02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Sequence Stratigraphic Study in Myazaki Group
Arbura formation (forced regressive sequences) kyushu, japan 2005 from KYI KHIN
]]> 554 3 https://cdn.slidesharecdn.com/ss_thumbnails/arburaformationforcedregressivesequenceskyushujapan2005-141115235656-conversion-gate02-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Presentation landslide (kyi khin et al , 2014) /slideshow/presentation-landslide-kyi-khin-et-al-2014-41608535/41608535 presentationlandslidekyikhinetal2014final-141115235508-conversion-gate01
Presentation at AUN-SEED-NET, University of Yangon, Myanmar 2014]]>
Presentation at AUN-SEED-NET, University of Yangon, Myanmar 2014]]> Sat, 15 Nov 2014 23:55:08 GMT /slideshow/presentation-landslide-kyi-khin-et-al-2014-41608535/41608535 kyikyaw2@slideshare.net(kyikyaw2) Presentation landslide (kyi khin et al , 2014) kyikyaw2 Presentation at AUN-SEED-NET, University of Yangon, Myanmar 2014 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/presentationlandslidekyikhinetal2014final-141115235508-conversion-gate01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation at AUN-SEED-NET, University of Yangon, Myanmar 2014
Presentation landslide (kyi khin et al , 2014) from KYI KHIN
]]> 901 1 https://cdn.slidesharecdn.com/ss_thumbnails/presentationlandslidekyikhinetal2014final-141115235508-conversion-gate01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 ?????¤ÎµØÙ|£¨English version) /slideshow/english-version-41608504/41608504 englishversion-141115235216-conversion-gate02
Presentation at Engineering geology Association, Kyushu Branch, Japan 2005]]>
Presentation at Engineering geology Association, Kyushu Branch, Japan 2005]]> Sat, 15 Nov 2014 23:52:16 GMT /slideshow/english-version-41608504/41608504 kyikyaw2@slideshare.net(kyikyaw2) ?????¤ÎµØÙ|£¨English version) kyikyaw2 Presentation at Engineering geology Association, Kyushu Branch, Japan 2005 <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/englishversion-141115235216-conversion-gate02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Presentation at Engineering geology Association, Kyushu Branch, Japan 2005
¥ß¥ã¥ó¥Þ©`¤ÎµØÙ|£¨English version) from KYI KHIN
]]> 1193 1 https://cdn.slidesharecdn.com/ss_thumbnails/englishversion-141115235216-conversion-gate02-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Rocks of Singapore (2013) /slideshow/rocks-of-singapore-2013-37593182/37593182 rocksofsingapore2013-140802020148-phpapp01
Some collection of Singapore Rocks and thin sections photo-micrographs]]>
Some collection of Singapore Rocks and thin sections photo-micrographs]]> Sat, 02 Aug 2014 02:01:48 GMT /slideshow/rocks-of-singapore-2013-37593182/37593182 kyikyaw2@slideshare.net(kyikyaw2) Rocks of Singapore (2013) kyikyaw2 Some collection of Singapore Rocks and thin sections photo-micrographs <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/rocksofsingapore2013-140802020148-phpapp01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Some collection of Singapore Rocks and thin sections photo-micrographs
Rocks of Singapore (2013) from KYI KHIN
]]> 1596 2 https://cdn.slidesharecdn.com/ss_thumbnails/rocksofsingapore2013-140802020148-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Field trip to Aso volcano, Kyushu, Japan /slideshow/field-trip-to-aso-volcano-kyushu-japan/18770505 fieldtriptoasovolcano-130414000153-phpapp02
A last Field trip before leave Japan 2003.]]>
A last Field trip before leave Japan 2003.]]> Sun, 14 Apr 2013 00:01:53 GMT /slideshow/field-trip-to-aso-volcano-kyushu-japan/18770505 kyikyaw2@slideshare.net(kyikyaw2) Field trip to Aso volcano, Kyushu, Japan kyikyaw2 A last Field trip before leave Japan 2003. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/fieldtriptoasovolcano-130414000153-phpapp02-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> A last Field trip before leave Japan 2003.
Field trip to Aso volcano, Kyushu, Japan from KYI KHIN
]]> 1094 2 https://cdn.slidesharecdn.com/ss_thumbnails/fieldtriptoasovolcano-130414000153-phpapp02-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Technical report on landslided, kyushu, japan (2006) in japanese /slideshow/technical-report-on-landslided-kyushu-japan-2006-in-japanese-15721766/15721766 technicalreportonlandslidedkyushujapan2006injapanese-121221015131-phpapp01
The Japan Archipelago is a part of the Circum Pacific Orogenic Belt and is geologically very unstable. The bedrock materials which comprise the mountain terrain have been severely fractured since its formation and have developed numerous fault fracture zones. Furthermore, the islands are located within the monsoon zone and receive abundant rainfall. Coupled with early summer rainy spells and later typhoons, numerous landslides occur resulting in staggering damages. The geological and geographical situations attribute important factors in Landslide Evolution and Landslide Topography. Among the slopes that have landslide topography, there are many Static Landslides (Old Landslides) with erosional features and dissected scarps caused many active landslides. Main factors of the Landslide and slope failures triggered by Typhoon No. 14 are heavy rainfall (1,322mm) and geologic characteristics of the earth materials formed by highly deformed Pre-Tertiary sedimentary rocks overlain by Quaternary un-welded pyroclastic deposits, Old Alluvial deposits with debris flows units. Major slope movements within these areas are represented by the failure of unwelded pyroclastic flow deposits and unconsolidated old alluvial deposits accompanied with intense rainfall. Furthermore, these failures involve not only the rapid slide with fall of the pyroclastic flow deposits, but also include the rapid slide of the tephra and thick older alluvial deposits underlain by the deformed bedrocks. Most of these Large Scale Landslide features form by an aggregate of Smaller Landslide features and that movement could facilitate infiltration of groundwater into the head portion and the flank of landslide mass. Such conditions can cause localized instability and result in the formation of smaller landslides within the large landslide. Many of the currently existing active landslides represent reactivated portions of an old larger landslide masses in the Southern Kyushu regions. Further, it has been speculated that the landslide topography and material compositions of earth materials could also be modified when changes in the ground water flow regime. Finally, we discussed the relationship between landslide topography, mode of movement and mitigation measures according to the characteristics of each slope failures. ]]>
The Japan Archipelago is a part of the Circum Pacific Orogenic Belt and is geologically very unstable. The bedrock materials which comprise the mountain terrain have been severely fractured since its formation and have developed numerous fault fracture zones. Furthermore, the islands are located within the monsoon zone and receive abundant rainfall. Coupled with early summer rainy spells and later typhoons, numerous landslides occur resulting in staggering damages. The geological and geographical situations attribute important factors in Landslide Evolution and Landslide Topography. Among the slopes that have landslide topography, there are many Static Landslides (Old Landslides) with erosional features and dissected scarps caused many active landslides. Main factors of the Landslide and slope failures triggered by Typhoon No. 14 are heavy rainfall (1,322mm) and geologic characteristics of the earth materials formed by highly deformed Pre-Tertiary sedimentary rocks overlain by Quaternary un-welded pyroclastic deposits, Old Alluvial deposits with debris flows units. Major slope movements within these areas are represented by the failure of unwelded pyroclastic flow deposits and unconsolidated old alluvial deposits accompanied with intense rainfall. Furthermore, these failures involve not only the rapid slide with fall of the pyroclastic flow deposits, but also include the rapid slide of the tephra and thick older alluvial deposits underlain by the deformed bedrocks. Most of these Large Scale Landslide features form by an aggregate of Smaller Landslide features and that movement could facilitate infiltration of groundwater into the head portion and the flank of landslide mass. Such conditions can cause localized instability and result in the formation of smaller landslides within the large landslide. Many of the currently existing active landslides represent reactivated portions of an old larger landslide masses in the Southern Kyushu regions. Further, it has been speculated that the landslide topography and material compositions of earth materials could also be modified when changes in the ground water flow regime. Finally, we discussed the relationship between landslide topography, mode of movement and mitigation measures according to the characteristics of each slope failures. ]]> Fri, 21 Dec 2012 01:51:31 GMT /slideshow/technical-report-on-landslided-kyushu-japan-2006-in-japanese-15721766/15721766 kyikyaw2@slideshare.net(kyikyaw2) Technical report on landslided, kyushu, japan (2006) in japanese kyikyaw2 The Japan Archipelago is a part of the Circum Pacific Orogenic Belt and is geologically very unstable. The bedrock materials which comprise the mountain terrain have been severely fractured since its formation and have developed numerous fault fracture zones. Furthermore, the islands are located within the monsoon zone and receive abundant rainfall. Coupled with early summer rainy spells and later typhoons, numerous landslides occur resulting in staggering damages. The geological and geographical situations attribute important factors in Landslide Evolution and Landslide Topography. Among the slopes that have landslide topography, there are many Static Landslides (Old Landslides) with erosional features and dissected scarps caused many active landslides. Main factors of the Landslide and slope failures triggered by Typhoon No. 14 are heavy rainfall (1,322mm) and geologic characteristics of the earth materials formed by highly deformed Pre-Tertiary sedimentary rocks overlain by Quaternary un-welded pyroclastic deposits, Old Alluvial deposits with debris flows units. Major slope movements within these areas are represented by the failure of unwelded pyroclastic flow deposits and unconsolidated old alluvial deposits accompanied with intense rainfall. Furthermore, these failures involve not only the rapid slide with fall of the pyroclastic flow deposits, but also include the rapid slide of the tephra and thick older alluvial deposits underlain by the deformed bedrocks. Most of these Large Scale Landslide features form by an aggregate of Smaller Landslide features and that movement could facilitate infiltration of groundwater into the head portion and the flank of landslide mass. Such conditions can cause localized instability and result in the formation of smaller landslides within the large landslide. Many of the currently existing active landslides represent reactivated portions of an old larger landslide masses in the Southern Kyushu regions. Further, it has been speculated that the landslide topography and material compositions of earth materials could also be modified when changes in the ground water flow regime. Finally, we discussed the relationship between landslide topography, mode of movement and mitigation measures according to the characteristics of each slope failures. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/technicalreportonlandslidedkyushujapan2006injapanese-121221015131-phpapp01-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The Japan Archipelago is a part of the Circum Pacific Orogenic Belt and is geologically very unstable. The bedrock materials which comprise the mountain terrain have been severely fractured since its formation and have developed numerous fault fracture zones. Furthermore, the islands are located within the monsoon zone and receive abundant rainfall. Coupled with early summer rainy spells and later typhoons, numerous landslides occur resulting in staggering damages. The geological and geographical situations attribute important factors in Landslide Evolution and Landslide Topography. Among the slopes that have landslide topography, there are many Static Landslides (Old Landslides) with erosional features and dissected scarps caused many active landslides. Main factors of the Landslide and slope failures triggered by Typhoon No. 14 are heavy rainfall (1,322mm) and geologic characteristics of the earth materials formed by highly deformed Pre-Tertiary sedimentary rocks overlain by Quaternary un-welded pyroclastic deposits, Old Alluvial deposits with debris flows units. Major slope movements within these areas are represented by the failure of unwelded pyroclastic flow deposits and unconsolidated old alluvial deposits accompanied with intense rainfall. Furthermore, these failures involve not only the rapid slide with fall of the pyroclastic flow deposits, but also include the rapid slide of the tephra and thick older alluvial deposits underlain by the deformed bedrocks. Most of these Large Scale Landslide features form by an aggregate of Smaller Landslide features and that movement could facilitate infiltration of groundwater into the head portion and the flank of landslide mass. Such conditions can cause localized instability and result in the formation of smaller landslides within the large landslide. Many of the currently existing active landslides represent reactivated portions of an old larger landslide masses in the Southern Kyushu regions. Further, it has been speculated that the landslide topography and material compositions of earth materials could also be modified when changes in the ground water flow regime. Finally, we discussed the relationship between landslide topography, mode of movement and mitigation measures according to the characteristics of each slope failures.
Technical report on landslided, kyushu, japan (2006) in japanese from KYI KHIN
]]> 902 2 https://cdn.slidesharecdn.com/ss_thumbnails/technicalreportonlandslidedkyushujapan2006injapanese-121221015131-phpapp01-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 https://cdn.slidesharecdn.com/profile-photo-kyikyaw2-48x48.jpg?cb=1548422343 Experienced in Geology and Engineering Geology fields for 15 years. Some areas covered Sedimentology, Sequence Stratigraphy and Tectonics of Myanmar, Japan, SE Asia regions and Engineering Geology. Some key performance in Geological Hazards investigation and Monitoring, Geological and Engineering Geological Mapping, Field Investigations and Soil and Rock Lab Testings paved ways to learn the role of a Geologist and Engineering Geologist in the field of Applied Geosciences. Recently, involving in Tunneling and Deep excavation Projects with Geotechnical and Engineering Geology scopes. http://www.myanmargeosciences.org https://cdn.slidesharecdn.com/ss_thumbnails/arakancoastalrangeskkkz2017-180121040255-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/arakan-coastal-ranges-kyi-khin-and-khin-zaw-2017pptx/86464121 Arakan coastal ranges,... https://cdn.slidesharecdn.com/ss_thumbnails/a9648d70-47cd-4e05-90b1-f3730b4b43c9-161112031734-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/role-of-geologists-in-natural-hazard-mapping-and-applicationdr-kyi-khinmgss-21st-annual-memorial-maganine-2016-68738347/68738347 Role of Geologists in ... https://cdn.slidesharecdn.com/ss_thumbnails/c871341a-2ccc-4fcc-910d-ba1c11f7d217-160921003012-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/outcrops-of-sgkk-klaugust-2016final200916/66236611 Outcrops of SG_KK &amp; KL...