Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin

The evaluation of post-mature source rocks gradually invalidates by traditional organic geochemical parameters due to the decreasing of organic matter abundance. However, the inorganic elements in source rocks are not easily affected by thermal evolution. In order to explore the application of inorg...

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Main Authors: Chunhua SHI, Shujiao SHAN, Jing HAO, Bing LUO, Jian CAO
Format: Article
Language:zho
Published: Editorial Office of Petroleum Geology and Experiment 2022-05-01
Series:Shiyou shiyan dizhi
Subjects:
Online Access:https://www.sysydz.net/cn/article/doi/10.11781/sysydz202203505
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author Chunhua SHI
Shujiao SHAN
Jing HAO
Bing LUO
Jian CAO
author_facet Chunhua SHI
Shujiao SHAN
Jing HAO
Bing LUO
Jian CAO
author_sort Chunhua SHI
collection DOAJ
description The evaluation of post-mature source rocks gradually invalidates by traditional organic geochemical parameters due to the decreasing of organic matter abundance. However, the inorganic elements in source rocks are not easily affected by thermal evolution. In order to explore the application of inorganic geochemical methods in the evaluation of post-mature source rocks, this paper takes the Sinian-Cambrian source rocks in the Sichuan Basin as an example to conduct an evaluation based on the inorganic (major, trace and rare earth elements) geochemistry method with three controlling factors of source rock development (paleoproductivity, sedimentary environment and sedimentary rate). The concentration of Ba and Ni, MoEF and UEF and Ce anomaly, and TiO2/Al2O3 ratio could be correlated with paleoproducitvity, sedimentary environment and sedimentary rate, respectively. The results showed that the enrichment of organic matter was mainly controlled by sedimentary environment and paleoproductivity, but are barely effected by sedimentary rate. Source rocks in the Lower Cambrian Qiongzhusi Formation in the central Sichuan and Weiyuan-Ziyang areas have high paleoproductivity and the most reduced environment and thus are one of the best quality source rocks. Therefore, inorganic geochemistry method is an effective way to evaluate postmature source rocks.
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spelling doaj.art-774337e2edf4423b8be967196d31e49b2024-03-05T04:31:16ZzhoEditorial Office of Petroleum Geology and ExperimentShiyou shiyan dizhi1001-61122022-05-0144350551410.11781/sysydz202203505sysydz-44-3-505Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan BasinChunhua SHI0Shujiao SHAN1Jing HAO2Bing LUO3Jian CAO4College of Resources and Environmental Engineering, Guizhou University, Guiyang, Guizhou 550025, ChinaExploration and Development Research Institute, PetroChina Southwest Oil and Gas Field Company, Chengdu, Sichuan 610041, ChinaChongqing Gas Mine, PetroChina Southwest Oil and Gas Field Company, Chongqing 401120, ChinaChongqing Gas Mine, PetroChina Southwest Oil and Gas Field Company, Chongqing 401120, ChinaSchool of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210023, ChinaThe evaluation of post-mature source rocks gradually invalidates by traditional organic geochemical parameters due to the decreasing of organic matter abundance. However, the inorganic elements in source rocks are not easily affected by thermal evolution. In order to explore the application of inorganic geochemical methods in the evaluation of post-mature source rocks, this paper takes the Sinian-Cambrian source rocks in the Sichuan Basin as an example to conduct an evaluation based on the inorganic (major, trace and rare earth elements) geochemistry method with three controlling factors of source rock development (paleoproductivity, sedimentary environment and sedimentary rate). The concentration of Ba and Ni, MoEF and UEF and Ce anomaly, and TiO2/Al2O3 ratio could be correlated with paleoproducitvity, sedimentary environment and sedimentary rate, respectively. The results showed that the enrichment of organic matter was mainly controlled by sedimentary environment and paleoproductivity, but are barely effected by sedimentary rate. Source rocks in the Lower Cambrian Qiongzhusi Formation in the central Sichuan and Weiyuan-Ziyang areas have high paleoproductivity and the most reduced environment and thus are one of the best quality source rocks. Therefore, inorganic geochemistry method is an effective way to evaluate postmature source rocks.https://www.sysydz.net/cn/article/doi/10.11781/sysydz202203505post-mature source rockinorganic geochemistryhydrocarbon generation capacitysource rock evaluationsiniancambriansichuan basin
spellingShingle Chunhua SHI
Shujiao SHAN
Jing HAO
Bing LUO
Jian CAO
Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
Shiyou shiyan dizhi
post-mature source rock
inorganic geochemistry
hydrocarbon generation capacity
source rock evaluation
sinian
cambrian
sichuan basin
title Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
title_full Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
title_fullStr Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
title_full_unstemmed Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
title_short Inorganic geochemical characteristics and evaluation of Sinian-Cambrian post-mature source rocks in Sichuan Basin
title_sort inorganic geochemical characteristics and evaluation of sinian cambrian post mature source rocks in sichuan basin
topic post-mature source rock
inorganic geochemistry
hydrocarbon generation capacity
source rock evaluation
sinian
cambrian
sichuan basin
url https://www.sysydz.net/cn/article/doi/10.11781/sysydz202203505
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AT shujiaoshan inorganicgeochemicalcharacteristicsandevaluationofsiniancambrianpostmaturesourcerocksinsichuanbasin
AT jinghao inorganicgeochemicalcharacteristicsandevaluationofsiniancambrianpostmaturesourcerocksinsichuanbasin
AT bingluo inorganicgeochemicalcharacteristicsandevaluationofsiniancambrianpostmaturesourcerocksinsichuanbasin
AT jiancao inorganicgeochemicalcharacteristicsandevaluationofsiniancambrianpostmaturesourcerocksinsichuanbasin