| 北黄海盆地东部坳陷不同物源影响下储层的成岩演化 |
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| 引用本文： | 高丹, 程日辉, 付秋林, 沈艳杰, 王嘹亮, 谭笑. 北黄海盆地东部坳陷不同物源影响下储层的成岩演化[J]. 海洋地质前沿, 2023, 39(3): 61-70. doi: 10.16028/j.1009-2722.2022.102 |
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| 作者姓名： | 高丹 程日辉 付秋林 沈艳杰 王嘹亮 谭笑 |
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| 作者单位： | 1.沈阳师范大学古生物学院 ，沈阳 110034; 2.自然资源部东北亚古生物演化重点实验室，沈阳 110034; 3.吉林大学地球科学学院，长春 130061; 4.辽宁省地质矿产研究院有限责任公司，沈阳 110000; 5.中国地质调查局广州海洋地质调查局，广州 511458 |
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| 基金项目： | 中国地质调查局项目（GZH200700405）；;国家自然科学基金（41902009）； |
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| 摘 要： | 以北黄海盆地东部坳陷中生界碎屑岩储层为研究对象，运用岩石薄片光学显微鉴定、阴极发光和扫描电镜等技术方法和手段分析成岩特征，探讨不同物源-沉积体系控制下储层的成岩演化。研究认为，东部坳陷中生界储层主要处于中成岩阶段A期，发育的主要成岩作用类型为压实作用、胶结作用、凝灰质脱玻化作用、交代作用、蚀变作用和溶蚀-溶解作用，其中，东部地区压实作用强度要高于西南和北部地区，北部地区碳酸盐胶结物的含量明显高于其他地区，东部地区以凝灰质胶结为特征并发生凝灰质脱玻化作用，西南部以黏土矿质胶结为特征并发生明显的黏土矿物转化现象，西南和北部地区的溶蚀/溶解作用的发育程度要好于东部地区。综合分析认为，研究区不同物源沉积区储层具有差异的成岩特征，表现为不同的储层序列，从而影响储层的成岩演化。
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| 关 键 词： | 北黄海盆地 中生界 储层 物质来源 成岩演化 |
| 收稿时间： | 2022-04-08 |
The evolution of diagenesis influenced by different provenance in the Eastern Depression of the North Yellow Sea Basin |
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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 |
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| Authors: | GAO Dan CHENG Rihui FU Qiulin SHEN Yanjie WANG Liaoliang TAN Xiao |
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| Affiliation: | 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 |
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| 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. |
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| Keywords: | North Yellow Sea Basin Mesozoic reservoir provenance evolution of diagenesis |
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