The evolution of diagenesis influenced by different provenance in the Eastern Depression of the North Yellow Sea Basin

GAO Dan; CHENG Rihui; FU Qiulin; SHEN Yanjie; WANG Liaoliang; TAN Xiao

doi:10.16028/j.1009-2722.2022.102

2023 Vol. 39, No. 3

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Article navigation > Marine Geology Frontiers > 2023 > 39(3): 61-70

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GAO Dan, CHENG Rihui, FU Qiulin, SHEN Yanjie, WANG Liaoliang, TAN Xiao. The evolution of diagenesis influenced by different provenance in the Eastern Depression of the North Yellow Sea Basin[J]. Marine Geology Frontiers, 2023, 39(3): 61-70. doi: 10.16028/j.1009-2722.2022.102

Citation:

GAO Dan, CHENG Rihui, FU Qiulin, SHEN Yanjie, WANG Liaoliang, TAN Xiao. The evolution of diagenesis influenced by different provenance in the Eastern Depression of the North Yellow Sea Basin[J]. Marine Geology Frontiers, 2023, 39(3): 61-70. doi: 10.16028/j.1009-2722.2022.102

The evolution of diagenesis influenced by different provenance in the Eastern Depression of the North Yellow Sea Basin

1.
College of Palaeontology, Shenyang Normal University, Shenyang 110034, China
2.
Key Laboratory of Evolution of Past Life in NE Asia, Ministry of Natural Resources of China, Shenyang 110034, China
3.
College of Earth Sciences, Jilin University, Changchun 130061, China
4.
Institution of Geological and Mineral Survey of Liaoning, Shenyang 110000, China
5.
Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China

More Information

Corresponding author: FU Qiulin, woshifuqiulin@163.com

Received Date: 08 April 2022

Publish Date: 28 March 2023

Abstract

Abstract

To understand the diagenetic evolution of the reservoir that is controlled by different provenance- sedimentary systems, the clastic reservoir of the Mesozoic deposits in the Eastern Depression of the North Yellow Sea Basin was anatomized. Methods of thin section identification, cathodoluminescence, and scanning electron microscope were used. Results shows that the Mesozoic reservoir in the depression is largely in the stage A of mesodiagenesis, and the main diagenesis types include compaction, cementation, replacement/alteration, and tuffaceous devitrification/dissolution. The level of compaction in the eastern region is higher than that in the southwest and northern regions. The content of carbonate cement in the northern region is much higher than that in other regions. The eastern region is characterized by tuffaceous cementation and tuffaceous devitrification; and the southwest is characterized by clay mineral cementation and obvious clay mineral transformation. The development degree of dissolution in the southwest and northern regions is higher than that in the eastern region. Comprehensive analysis shows that the reservoirs in different provenance sedimentary areas in the study area have different diagenetic characteristics and show different reservoir sequences, which affected the diagenetic evolution of the reservoirs.
- North Yellow Sea Basin /
- Mesozoic /
- reservoir /
- provenance /
- evolution of diagenesis

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References

[1]	高丹,程日辉,沈艳杰,等. 北黄海盆地东部坳陷侏罗纪西南物源-沉积体系与源区构造背景分析[J]. 地球科学,2016,41(7):1171-1178. Google Scholar
[2]	宋雪,程日辉,高丹,等. 北黄海盆地东部坳陷侏罗纪北部物源-沉积体系的岩矿特征[J]. 世界地质,2015,34(4):1002-1012. doi: 10.3969/j.issn.1004-5589.2015.04.012 CrossRef Google Scholar
[3]	GAO D,CHENG R H,SHEN Y J,et al. Weathered and volcanic provenance-sedimentary system and its influence on reservoir quality in the east of the Eastern Depression,the North Yellow Sea Basin[J]. Earth Science,2018,2:353-368. Google Scholar
[4]	李文勇,李东旭,夏斌,等. 北黄海盆地构造演化特征分析[J]. 现代地质,2006,20(2):268-276. doi: 10.3969/j.issn.1000-8527.2006.02.010 CrossRef Google Scholar
[5]	王改云,刘金萍,王后金,等. 北黄海盆地东部坳陷中生界沉积特征及演化[J]. 沉积学报,2015,33(3):561-567. doi: 10.14027/j.cnki.cjxb.2015.03.014 CrossRef Google Scholar
[6]	蔡乾忠. 横贯黄海的中朝造山带与北、南黄海成盆成烃关系[J]. 石油与天然气地质,2005,26(2):185-192, 196. doi: 10.3321/j.issn:0253-9985.2005.02.010 CrossRef Google Scholar
[7]	胡小强,刘振湖,陈玲,等. 北黄海盆地某研究区块钻井层序地层及沉积特征[J]. 海洋地质与第四纪地质,2009,20(2):103-110. Google Scholar
[8]	杨艳秋,戴春山,刘万洙. 北黄海盆地基底结构特征[J]. 海洋地质动态,2003,19(5):25-56. doi: 10.3969/j.issn.1009-2722.2003.05.007 CrossRef Google Scholar
[9]	MASSOUD M S,KILLOPS S D,SCOTT A C,et al. Oil source rock potential of the lacustrine Jurassic Sim Uuju Formation,West Korea Bay Basin; PartⅠ:oil-source rock correlation and environment of deposition[J]. Journal of Petroleum Geoligy,1991,14(4):365-386. doi: 10.1111/j.1747-5457.1991.tb01032.x CrossRef Google Scholar
[10]	龚承林,雷怀彦,王英民,等. 北黄海盆地东部坳陷构造演化与油气地质特征[J]. 海洋地质与第四纪地质,2009,29(1):79-86. Google Scholar
[11]	梁世友,李凤丽,付洁,等. 北黄海盆地中生界烃源岩评价[J]. 石油实验地质,2009,31(3):249-252. doi: 10.3969/j.issn.1001-6112.2009.03.008 CrossRef Google Scholar
[12]	刘金萍,王嘹亮,简晓玲,等. 北黄海盆地中生界原油特征及油源初探[J]. 新疆石油地质,2013,34(5):515-518. Google Scholar
[13]	王强,王应斌,张友. 北黄海东部坳陷中生界储层特征[J]. 沉积与特提斯地质,2010,30(4):97-103. doi: 10.3969/j.issn.1009-3850.2010.04.015 CrossRef Google Scholar
[14]	梁杰,温珍河,肖国林,等. 北黄海盆地东部坳陷储层特征及影响因素[J]. 海洋地质与第四纪地质,2013,33(2):111-119. Google Scholar
[15]	刘振湖,高红芳,胡小强,等. 北黄海盆地东部坳陷中生界含油气系统研究[J]. 中国海上油气,2007,19(4):229-233. doi: 10.3969/j.issn.1673-1506.2007.04.003 CrossRef Google Scholar
[16]	高丹,程日辉,沈艳杰,等. 北黄海盆地东部坳陷中生界次生孔隙的发育规律[J]. 海洋地质与第四纪地质,2021,41(5):194-201. doi: 10.16562/j.cnki.0256-1492.2020121601 CrossRef Google Scholar
[17]	金仁植,费琪,杨香华,等. 北黄海盆地含油气系统与勘探前景[J]. 石油实验地质,2006(5):445-449,457. doi: 10.3969/j.issn.1001-6112.2006.05.008 CrossRef Google Scholar
[18]	陈玲,白志琳,李文勇. 北黄海盆地中新生代沉积坳陷特征及其油气勘探方向[J]. 石油物探,2006,45(3):319-323. doi: 10.3969/j.issn.1000-1441.2006.03.021 CrossRef Google Scholar
[19]	赵海玲,黄微,王成,等. 火山岩中脱玻化孔及其对储层的贡献[J]. 石油与天然气地质,2009,30(1):47-52,58. doi: 10.3321/j.issn:0253-9985.2009.01.007 CrossRef Google Scholar
[20]	张善文. 成岩过程中的“耗水作用”及其石油地质意义[J]. 沉积学报,2007,25(5):701-707. doi: 10.3969/j.issn.1000-0550.2007.05.007 CrossRef Google Scholar
[21]	PARKER A,SELLWOOD B W. Sediment Diagenesis \|\| Diagenetic Reactions in Sandstones[J]. Norwegian:D. Reidel Publishing Company,1981:215-269. Google Scholar
[22]	PALMER M R,ELDERFIELD H. Sr isotope composition of sea water over the past 75Myr[J]. Nature,1985,314(6011):526-528. doi: 10.1038/314526a0 CrossRef Google Scholar
[23]	WIGNALL P B,TWITCHETT R J. Oceanic anoxia and the end Permian mass extinction[J]. Science,1996,272(5265):1155-1158. doi: 10.1126/science.272.5265.1155 CrossRef Google Scholar
[24]	KIMURA H,WATANABE Y. Ocean anoxia at the Precambrian-Cambrian boundary[J]. Geology,2001,29(11):995-998. doi: 10.1130/0091-7613(2001)029<0995:OAATPC>2.0.CO;2 CrossRef Google Scholar
[25]	王璞珺,高有峰,任延广,等. 松辽盆地青山口组橄榄组安岩:40Ar/39Ar 年龄、地球化学及其成盆、成烃和成藏意义[J]. 岩石学报,2009,25(5):1178-1190. Google Scholar
[26]	蒋宜勤,柳益群,杨召,等. 准噶尔盆地吉木萨尔凹陷凝灰岩型致密油特征与成因[J]. 石油勘探与开发,2015,42(6):741-749. Google Scholar
[27]	MANGO F D,HIGHTOWER J W,Alan A T. Role of transition-metal catalysis in the formation of natural gas[J]. Nature,1994,368(6):536-538. Google Scholar
[28]	金强,熊寿生,卢培德. 中国断陷盆地主要生油岩中的火山活动及其意义[J]. 地质论评,1998,44(2):136-142. doi: 10.3321/j.issn:0371-5736.1998.02.004 CrossRef Google Scholar
[29]	MANGO F D. The carbon isotopic composition of catalytic gas:a comparative analysis with natural gas[J]. Geochim. Cosmochim. Acta,1999,63(7):1097-1106. Google Scholar
[30]	程日辉,王璞珺,刘万洙,等. 构造活动和火山作用对干酪根成烃转化的影响[J]. 地质科技情报,2003,22(1):83-87. Google Scholar