Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China

Super-large natural gas fields have been discovered in the deep and ultra-deep layers of onshore and offshore petroliferous basins in China since the beginning of the 21st century, and the geological conditions for the formation of these gas fields and their development laws have already been discus...

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Main Authors: Wei Li, Ziliang Yu, Xueke Wang, Zhichao Yu, Xuesong Lu, Qingfu Feng
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2020-10-01
Series:Natural Gas Industry B
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2352854020300838
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author Wei Li
Ziliang Yu
Xueke Wang
Zhichao Yu
Xuesong Lu
Qingfu Feng
author_facet Wei Li
Ziliang Yu
Xueke Wang
Zhichao Yu
Xuesong Lu
Qingfu Feng
author_sort Wei Li
collection DOAJ
description Super-large natural gas fields have been discovered in the deep and ultra-deep layers of onshore and offshore petroliferous basins in China since the beginning of the 21st century, and the geological conditions for the formation of these gas fields and their development laws have already been discussed in a large number of literatures, but the relationship between over pressure and the formation of this kind of gas fields is still less researched. In this regard, this paper firstly analyzed the gas reservoir development law, sealing conditions and over pressure characteristics of deep and ultra-deep super-large gas fields. Then, the formation mechanisms of deep and ultra-deep over pressure caprocks were investigated and the development law of deep and ultra-deep super-large gas fields and their relationship with over pressure caprocks were discussed. Finally, the favorable areas for the next exploration of deep and ultra-deep natural gas were pointed out. And the following research results were obtained. First, the formation of deep and ultra-deep super-large gas fields is closely related to the development of over pressure caprocks. Over pressure caprock is a necessary condition for the formation of deep and ultra-deep super-large gas fields, and there are three over pressure formation mechanisms, including pressure seal of salt-gypsum layer, pressure seal of residual uplift and pressure seal of hydrocarbon-generating pressurization. Second, as for deep and ultra-deep over pressure caprocks and super-large gas fields, there are four reservoir–caprock assemblage modes under different pressure environments, i.e., over pressure salt-gypsum seal and over pressure super-large gas field (Type I), internal over pressure compartment and over pressure super-large gas field (Type II), high-pressure argillaceous shale seal at the bottom of over pressure compartment and normal-pressure super-larger gas field (Type III), and over pressure source rock seal and normal-pressure super-larger gas field (Type IV). In conclusion, there are Type I super-large gas fields in the Kuqa Depression of the Tarim Basin, types II and III in the Junggar Basin, types I–IV in the Sichuan Basin and Type IV in the Bohai Bay Basin.
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spelling doaj.art-56f184d906a74bf88f35d6256e3411b92024-03-02T11:13:26ZengKeAi Communications Co., Ltd.Natural Gas Industry B2352-85402020-10-0175443452Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of ChinaWei Li0Ziliang Yu1Xueke Wang2Zhichao Yu3Xuesong Lu4Qingfu Feng5PetroChina Research Institute of Petroleum Exploration and Development, Beijing, 100083, China; Corresponding author.Beijing Research Center, CNOOC China Limited, Beijing, 100011, ChinaPetroChina Research Institute of Petroleum Exploration and Development, Beijing, 100083, ChinaPetroChina Research Institute of Petroleum Exploration and Development, Beijing, 100083, ChinaPetroChina Research Institute of Petroleum Exploration and Development, Beijing, 100083, ChinaPetroChina Research Institute of Petroleum Exploration and Development, Beijing, 100083, ChinaSuper-large natural gas fields have been discovered in the deep and ultra-deep layers of onshore and offshore petroliferous basins in China since the beginning of the 21st century, and the geological conditions for the formation of these gas fields and their development laws have already been discussed in a large number of literatures, but the relationship between over pressure and the formation of this kind of gas fields is still less researched. In this regard, this paper firstly analyzed the gas reservoir development law, sealing conditions and over pressure characteristics of deep and ultra-deep super-large gas fields. Then, the formation mechanisms of deep and ultra-deep over pressure caprocks were investigated and the development law of deep and ultra-deep super-large gas fields and their relationship with over pressure caprocks were discussed. Finally, the favorable areas for the next exploration of deep and ultra-deep natural gas were pointed out. And the following research results were obtained. First, the formation of deep and ultra-deep super-large gas fields is closely related to the development of over pressure caprocks. Over pressure caprock is a necessary condition for the formation of deep and ultra-deep super-large gas fields, and there are three over pressure formation mechanisms, including pressure seal of salt-gypsum layer, pressure seal of residual uplift and pressure seal of hydrocarbon-generating pressurization. Second, as for deep and ultra-deep over pressure caprocks and super-large gas fields, there are four reservoir–caprock assemblage modes under different pressure environments, i.e., over pressure salt-gypsum seal and over pressure super-large gas field (Type I), internal over pressure compartment and over pressure super-large gas field (Type II), high-pressure argillaceous shale seal at the bottom of over pressure compartment and normal-pressure super-larger gas field (Type III), and over pressure source rock seal and normal-pressure super-larger gas field (Type IV). In conclusion, there are Type I super-large gas fields in the Kuqa Depression of the Tarim Basin, types II and III in the Junggar Basin, types I–IV in the Sichuan Basin and Type IV in the Bohai Bay Basin.http://www.sciencedirect.com/science/article/pii/S2352854020300838Deep layerUltra-deep layerOverpressure caprockFormation mechanismSuper-large gas fieldTarim Basin
spellingShingle Wei Li
Ziliang Yu
Xueke Wang
Zhichao Yu
Xuesong Lu
Qingfu Feng
Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
Natural Gas Industry B
Deep layer
Ultra-deep layer
Overpressure caprock
Formation mechanism
Super-large gas field
Tarim Basin
title Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
title_full Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
title_fullStr Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
title_full_unstemmed Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
title_short Formation mechanisms of deep and ultra-deep over pressure caprocks and their relationships with super-large gas fields in the petroliferous basins of China
title_sort formation mechanisms of deep and ultra deep over pressure caprocks and their relationships with super large gas fields in the petroliferous basins of china
topic Deep layer
Ultra-deep layer
Overpressure caprock
Formation mechanism
Super-large gas field
Tarim Basin
url http://www.sciencedirect.com/science/article/pii/S2352854020300838
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