Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation

Based on organic petrology, organic geochemistry and SEM method, type, formation period and source of bitumens in the Cambrian Longwangmiao Formation in the central Sichuan Basin were well investigated, and combined with fluid inclusions and tectonic evolution characteristics, the hydrocarbon accumu...

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Main Authors: Bin Hao, Wenzhi Zhao, Suyun Hu, Shuyuan Shi, Ping Gao, Tongshan Wang, Shipeng Huang, Hua Jiang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2018-03-01
Series:Petroleum Research
Online Access:http://www.sciencedirect.com/science/article/pii/S2096249518300231
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spelling doaj-48e3a88394ce4a708ff15b3d642cc8fa2020-11-25T00:00:29ZengKeAi Communications Co., Ltd.Petroleum Research2096-24952018-03-01314456Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulationBin Hao0Wenzhi Zhao1Suyun Hu2Shuyuan Shi3Ping Gao4Tongshan Wang5Shipeng Huang6Hua Jiang7Northwest Branch, PetroChina Research Institute of Petroleum Exploration and Development, Gansu 730020, China; Corresponding author.PetroChina 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, ChinaSinopec Petroleum Exploration and Production Research Institute, 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, ChinaBased on organic petrology, organic geochemistry and SEM method, type, formation period and source of bitumens in the Cambrian Longwangmiao Formation in the central Sichuan Basin were well investigated, and combined with fluid inclusions and tectonic evolution characteristics, the hydrocarbon accumulation history of the gas reservoir of the Longwangmiao Formation in the Anyue gasfield was also studied. The result shows that all bitumens in the Longwangmiao Formation was from the Lower Cambrian source rocks, it had multiple genetic types which was dominated by the pyrolysis genetic type; the bitumens were formed into three stages, i.e., the bitumen of the oxidized water-washing type in the first stage, the bitumen of the precipitated type in the second stage, and the bitumen of the pyrolyzed type in the third stage; the gas reservoir in the Anyue gasfield experienced five stages of hydrocarbon charging, including two stages of liquid hydrocarbon charging, charging of the kerogen pyrolysis gas in the Late Triassic-Early Jurassic, charging of the crude oil pyrolysis gas in the Late Jurassic-Early Cretaceous and charging of the dry gas charging in the Himalayan trap reformation and adjustment process. Keywords: Bitumen, Biomarker, Authigenic minerals, Inclusion, Hydrocarbon charging, Longwangmiao Formation, Central Sichuanhttp://www.sciencedirect.com/science/article/pii/S2096249518300231
collection DOAJ
language English
format Article
sources DOAJ
author Bin Hao
Wenzhi Zhao
Suyun Hu
Shuyuan Shi
Ping Gao
Tongshan Wang
Shipeng Huang
Hua Jiang
spellingShingle Bin Hao
Wenzhi Zhao
Suyun Hu
Shuyuan Shi
Ping Gao
Tongshan Wang
Shipeng Huang
Hua Jiang
Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
Petroleum Research
author_facet Bin Hao
Wenzhi Zhao
Suyun Hu
Shuyuan Shi
Ping Gao
Tongshan Wang
Shipeng Huang
Hua Jiang
author_sort Bin Hao
title Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
title_short Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
title_full Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
title_fullStr Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
title_full_unstemmed Bitumen formation of Cambrian Longwangmiao Formation in the central Sichuan and its implication for hydrocarbon accumulation
title_sort bitumen formation of cambrian longwangmiao formation in the central sichuan and its implication for hydrocarbon accumulation
publisher KeAi Communications Co., Ltd.
series Petroleum Research
issn 2096-2495
publishDate 2018-03-01
description Based on organic petrology, organic geochemistry and SEM method, type, formation period and source of bitumens in the Cambrian Longwangmiao Formation in the central Sichuan Basin were well investigated, and combined with fluid inclusions and tectonic evolution characteristics, the hydrocarbon accumulation history of the gas reservoir of the Longwangmiao Formation in the Anyue gasfield was also studied. The result shows that all bitumens in the Longwangmiao Formation was from the Lower Cambrian source rocks, it had multiple genetic types which was dominated by the pyrolysis genetic type; the bitumens were formed into three stages, i.e., the bitumen of the oxidized water-washing type in the first stage, the bitumen of the precipitated type in the second stage, and the bitumen of the pyrolyzed type in the third stage; the gas reservoir in the Anyue gasfield experienced five stages of hydrocarbon charging, including two stages of liquid hydrocarbon charging, charging of the kerogen pyrolysis gas in the Late Triassic-Early Jurassic, charging of the crude oil pyrolysis gas in the Late Jurassic-Early Cretaceous and charging of the dry gas charging in the Himalayan trap reformation and adjustment process. Keywords: Bitumen, Biomarker, Authigenic minerals, Inclusion, Hydrocarbon charging, Longwangmiao Formation, Central Sichuan
url http://www.sciencedirect.com/science/article/pii/S2096249518300231
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