Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I)
By using a large amount of geological and geophysical data, the geological characteristics such as lithofacies and paleogeography of 4981 geological units at thirteen key geological periods or epoches since the Precambrian in the world have been figured out. The global lithofacies and paleogeography...
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KeAi Communications Co., Ltd.
2019-08-01
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Series: | Petroleum Exploration and Development |
Online Access: | http://www.sciencedirect.com/science/article/pii/S1876380419602259 |
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author | Guangya ZHANG Xiaoguang TONG Renchen XIN Zhixin WEN Feng MA Tongfei HUANG Zhaoming WANG Bingsong YU Yuejun LI Hanlin CHEN Xiaobing LIU Zuodong LIU |
author_facet | Guangya ZHANG Xiaoguang TONG Renchen XIN Zhixin WEN Feng MA Tongfei HUANG Zhaoming WANG Bingsong YU Yuejun LI Hanlin CHEN Xiaobing LIU Zuodong LIU |
author_sort | Guangya ZHANG |
collection | DOAJ |
description | By using a large amount of geological and geophysical data, the geological characteristics such as lithofacies and paleogeography of 4981 geological units at thirteen key geological periods or epoches since the Precambrian in the world have been figured out. The global lithofacies and paleogeography charts have been compiled by ArcGis mapping technology. Combined with the results of plate-paleogeography reconstruction, the lithofacies and paleogeography as well as the prototype basins of these global paleoplates have been restored with the Gplate software. Results show that there are 22 kinds of lithofacies combinations and 10 types of paleogeography units developed since Precambrian. These features of lithofacies and paleogeography as well as their evolution were mainly controlled by the divergent and convergent movements of those plates. Taking the results of the lithofacis and paleogeography at the present and paleoplate location during the seven key geological periods from the Precambrian to Paleozoic for example, during the Late Precambrian and Cambrian, the large-scale disintegration of the Rodinia supercontinent resulted in reduction of uplift denudation area and clastic terrestrial facies area, the expansion of coastal-shallow marine facies and shallow-water carbonate platform. In Devonian, uplift denudation area and clastic terrestrial facies area began to increase and littoral-shallow marine facies area and shallow-water carbonate platform shrank as a result of the formation of Larussia supercontinent. In the Permian, with the formation of the Pangea continent, the development of the global uplift denudation area and clastic terrestrial facies reached its peak, while the littoral and shallow marine facies were very limited in distribution. The lithofacies and paleogeography features and evolution patterns of different stages lay a solid foundation for analyzing the formation conditions of geological elements, such as source rocks, reservoirs and cap rocks for oil and gas accumulation, and revealing the distribution regularity of oil and gas around the world. Key words: global, lithofacies and paleogeography, paleogeography map, plate tectonics, prototype basin, tectonic evolution, lithofacies assemblage, oil and gas distribution |
first_indexed | 2024-12-17T03:53:31Z |
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institution | Directory Open Access Journal |
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spelling | doaj.art-78ae25fbc0c54eec9a9492e2628d1f512022-12-21T22:04:41ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042019-08-01464664686Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I)Guangya ZHANG0Xiaoguang TONG1Renchen XIN2Zhixin WEN3Feng MA4Tongfei HUANG5Zhaoming WANG6Bingsong YU7Yuejun LI8Hanlin CHEN9Xiaobing LIU10Zuodong LIU11Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaChina National Oil and Gas Exploration and Development Company Ltd., Beijing 100034, ChinaChina University of Geosciences, Beijing 100083, ChinaResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China; Corresponding authorResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaChina University of Geosciences, Beijing 100083, ChinaInstitute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaZhejiang University, Hangzhou 310058, ChinaResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaResearch Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, ChinaBy using a large amount of geological and geophysical data, the geological characteristics such as lithofacies and paleogeography of 4981 geological units at thirteen key geological periods or epoches since the Precambrian in the world have been figured out. The global lithofacies and paleogeography charts have been compiled by ArcGis mapping technology. Combined with the results of plate-paleogeography reconstruction, the lithofacies and paleogeography as well as the prototype basins of these global paleoplates have been restored with the Gplate software. Results show that there are 22 kinds of lithofacies combinations and 10 types of paleogeography units developed since Precambrian. These features of lithofacies and paleogeography as well as their evolution were mainly controlled by the divergent and convergent movements of those plates. Taking the results of the lithofacis and paleogeography at the present and paleoplate location during the seven key geological periods from the Precambrian to Paleozoic for example, during the Late Precambrian and Cambrian, the large-scale disintegration of the Rodinia supercontinent resulted in reduction of uplift denudation area and clastic terrestrial facies area, the expansion of coastal-shallow marine facies and shallow-water carbonate platform. In Devonian, uplift denudation area and clastic terrestrial facies area began to increase and littoral-shallow marine facies area and shallow-water carbonate platform shrank as a result of the formation of Larussia supercontinent. In the Permian, with the formation of the Pangea continent, the development of the global uplift denudation area and clastic terrestrial facies reached its peak, while the littoral and shallow marine facies were very limited in distribution. The lithofacies and paleogeography features and evolution patterns of different stages lay a solid foundation for analyzing the formation conditions of geological elements, such as source rocks, reservoirs and cap rocks for oil and gas accumulation, and revealing the distribution regularity of oil and gas around the world. Key words: global, lithofacies and paleogeography, paleogeography map, plate tectonics, prototype basin, tectonic evolution, lithofacies assemblage, oil and gas distributionhttp://www.sciencedirect.com/science/article/pii/S1876380419602259 |
spellingShingle | Guangya ZHANG Xiaoguang TONG Renchen XIN Zhixin WEN Feng MA Tongfei HUANG Zhaoming WANG Bingsong YU Yuejun LI Hanlin CHEN Xiaobing LIU Zuodong LIU Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) Petroleum Exploration and Development |
title | Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) |
title_full | Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) |
title_fullStr | Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) |
title_full_unstemmed | Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) |
title_short | Evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide (I) |
title_sort | evolution of lithofacies and paleogeography and hydrocarbon distribution worldwide i |
url | http://www.sciencedirect.com/science/article/pii/S1876380419602259 |
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