Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China
Abstract Hydrocarbon-producing lacustrine basins are widely developed in the world, and China has a large number of lacustrine basins that have developed since the early Permian. The organic-rich shale-dominated heterogeneous source rock intervals in Chinese lacustrine basins generally contain frequ...
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Format: | Article |
Language: | English |
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KeAi Communications Co., Ltd.
2017-07-01
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Series: | Petroleum Science |
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Online Access: | http://link.springer.com/article/10.1007/s12182-017-0179-9 |
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author | Shu Jiang You-Liang Feng Lei Chen Yue Wu Zheng-Yu Xu Zheng-Long Jiang Dong-Sheng Zhou Dong-Sheng Cai Elinda McKenna |
author_facet | Shu Jiang You-Liang Feng Lei Chen Yue Wu Zheng-Yu Xu Zheng-Long Jiang Dong-Sheng Zhou Dong-Sheng Cai Elinda McKenna |
author_sort | Shu Jiang |
collection | DOAJ |
description | Abstract Hydrocarbon-producing lacustrine basins are widely developed in the world, and China has a large number of lacustrine basins that have developed since the early Permian. The organic-rich shale-dominated heterogeneous source rock intervals in Chinese lacustrine basins generally contain frequent thin interbeds of stratigraphically associated sandstone, siltstone, marl, dolomite, and limestone. The concept of “Hybrid Plays” as put forth in this article recognizes this pattern of alternating organic-rich shale and organic-lean interbeds and existence of mixed unconventional and conventional plays. Hybrid Plays in lacustrine source rock intervals present a unique closed petroleum system hosting continuous hydrocarbons. The interbedded organic-lean siliciclastic and/or carbonate plays are efficiently charged with hydrocarbons via short migration pathways from the adjacent organic-rich shale that is often also a self-sourced play. We assert “Hybrid Plays” provide the most realistic exploration model for targeting multiple-stacked and genetically related very tight shale, tight and conventional plays together in the entire source rock interval rather than individual plays only. The Hybrid Play model has been proven and works for a wide variety of lacustrine rift, sag and foreland basins in China. |
first_indexed | 2024-12-19T22:34:21Z |
format | Article |
id | doaj.art-7d4e500db8d042dd80a4d055b814e395 |
institution | Directory Open Access Journal |
issn | 1672-5107 1995-8226 |
language | English |
last_indexed | 2024-12-19T22:34:21Z |
publishDate | 2017-07-01 |
publisher | KeAi Communications Co., Ltd. |
record_format | Article |
series | Petroleum Science |
spelling | doaj.art-7d4e500db8d042dd80a4d055b814e3952022-12-21T20:03:16ZengKeAi Communications Co., Ltd.Petroleum Science1672-51071995-82262017-07-0114345948310.1007/s12182-017-0179-9Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in ChinaShu Jiang0You-Liang Feng1Lei Chen2Yue Wu3Zheng-Yu Xu4Zheng-Long Jiang5Dong-Sheng Zhou6Dong-Sheng Cai7Elinda McKenna8Energy and Geoscience Institute, University of UtahResearch Institute of Petroleum Exploration and Development, PetroChinaSchool of Geoscience and Technology, Southwest Petroleum UniversitySinopec Petroleum Exploration and Production Research InstitutePetroChina Hangzhou Institute of GeologySchool of Ocean Sciences, China University of GeosciencesSchool of Ocean Sciences, China University of GeosciencesCNOOCEnergy and Geoscience Institute, University of UtahAbstract Hydrocarbon-producing lacustrine basins are widely developed in the world, and China has a large number of lacustrine basins that have developed since the early Permian. The organic-rich shale-dominated heterogeneous source rock intervals in Chinese lacustrine basins generally contain frequent thin interbeds of stratigraphically associated sandstone, siltstone, marl, dolomite, and limestone. The concept of “Hybrid Plays” as put forth in this article recognizes this pattern of alternating organic-rich shale and organic-lean interbeds and existence of mixed unconventional and conventional plays. Hybrid Plays in lacustrine source rock intervals present a unique closed petroleum system hosting continuous hydrocarbons. The interbedded organic-lean siliciclastic and/or carbonate plays are efficiently charged with hydrocarbons via short migration pathways from the adjacent organic-rich shale that is often also a self-sourced play. We assert “Hybrid Plays” provide the most realistic exploration model for targeting multiple-stacked and genetically related very tight shale, tight and conventional plays together in the entire source rock interval rather than individual plays only. The Hybrid Play model has been proven and works for a wide variety of lacustrine rift, sag and foreland basins in China.http://link.springer.com/article/10.1007/s12182-017-0179-9Lacustrine basinHybrid PlaysShaleInterbedSource rockPetroleum system |
spellingShingle | Shu Jiang You-Liang Feng Lei Chen Yue Wu Zheng-Yu Xu Zheng-Long Jiang Dong-Sheng Zhou Dong-Sheng Cai Elinda McKenna Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China Petroleum Science Lacustrine basin Hybrid Plays Shale Interbed Source rock Petroleum system |
title | Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China |
title_full | Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China |
title_fullStr | Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China |
title_full_unstemmed | Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China |
title_short | Multiple-stacked Hybrid Plays of lacustrine source rock intervals: Case studies from lacustrine basins in China |
title_sort | multiple stacked hybrid plays of lacustrine source rock intervals case studies from lacustrine basins in china |
topic | Lacustrine basin Hybrid Plays Shale Interbed Source rock Petroleum system |
url | http://link.springer.com/article/10.1007/s12182-017-0179-9 |
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