川东地区下侏罗统自流井组东岳庙段泥页岩沉积特征及物质来源

doi:10.12108/yxyqc.20240411

岩性油气藏 ›› 2024, Vol. 36 ›› Issue (4): 122–135.doi: 10.12108/yxyqc.20240411

川东地区下侏罗统自流井组东岳庙段泥页岩沉积特征及物质来源

邹连松¹, 徐文礼^1,2, 梁西文³, 刘皓天³, 周坤⁴, 霍飞⁵, 周林³, 文华国^1,6

1. 成都理工大学沉积地质研究院, 成都 610059;
2. 宜宾学院工业化城市二氧化碳捕集封存与资源利用研究院, 四川宜宾 644000;
3. 中国石化江汉油田分公司勘探开发研究院, 武汉 430223;
4. 中国石油西南油气田公司川东北气矿, 四川达州 635000;
5. 西南石油大学地球科学与技术学院, 成都 610500;
6. 中石油集团碳酸盐岩储层重点实验室成都理工大学分室, 成都 610059

收稿日期:2023-06-25 修回日期:2023-08-13 出版日期:2024-07-01 发布日期:2024-07-04
第一作者:邹连松（1995—），男，成都理工大学在读硕士研究生，研究方向为沉积地质学。地址：（610059）成都市成华区二仙桥东三路1号成都理工大学。E-mail：zouliansong9@163.com。
通信作者: 徐文礼（1982—），男，副教授，主要从事储层沉积学教学和研究。E-mail:xuwenli5@163.com。
基金资助:
四川省天然气成藏物质基础青年科技创新团队基金（编号：2022JDTD0004）资助。

Sedimentary characteristics and sources of shale of Dongyuemiao member of Lower Jurassic Ziliujing Formation in eastern Sichuan Basin

ZOU Liansong¹, XUWenli^1,2, LIANG Xiwen³, LIU Haotian³, ZHOU Kun⁴, HOU Fei⁵, ZHOU Lin³, WEN Huaguo^1,6

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China;
2. Institute of Carbon Dioxide Capture and Storage & Resource Utilization in Industrial Cities, Yibin University, Yibin 644000, Sichuan, China;
3. Research Institute of Exploration and Development, Sinopec Jianghan Oilfield Company, Wuhan 430223, China;
4. Northeast Sichuan Gas District, PetroChina Southwest Oil and Gas Field Company, Dazhou 635000, Sichuan, China;
5. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
6. Key Laboratory of Carbonate Reservoir, CNPC, Chengdu University of Technology, Chengdu 610059, China

Received:2023-06-25 Revised:2023-08-13 Online:2024-07-01 Published:2024-07-04

摘要/Abstract

摘要： 川东地区下侏罗统自流井组东岳庙段发育一套深色泥页岩，具有较大的页岩气资源勘探开发潜力。将宏观大地构造背景与微观岩石学特征分析相结合，利用微量元素（包括稀土元素）数据，对川东地区下侏罗统自流井组东岳庙段泥页岩的沉积环境和物质来源进行了分析与讨论。研究结果表明：①川东地区下侏罗统东岳庙段自下而上依次沉积灰色介壳灰岩、灰色粉砂质泥岩、深灰色介壳泥岩、灰黑色页岩、灰—深灰色泥岩。②研究区东岳庙段泥页岩稀土元素总体具有轻稀土元素富集、重稀土元素亏损的特征，δCe 为负异常，Ce_anom平均值为 -0.015，V（/ V+Ni）平均值为 0.70，Sr/Cu 平均值为 2.43，Sr/Ba平均值为 0.16，（La/Yb）_N 平均值为 1.32，泥页岩沉积环境为相对贫氧的弱还原环境，整体为温暖湿润气候下的淡水沉积，且沉积速率较快，有利于有机质的富集和保存。③Zr/Sc-Th/Sc图和La/Sc-Co/Th图显示研究区沉积物母岩为花岗岩；Th/Sc 值为 0.78、Th/Co 值为 0.65、Th/Cr 值为 0.14、La/Sc 值为 2.14，均接近上地壳的相应元素比值，表明母岩主要为来自上地壳；La，Ce元素校正后平均质量分数分别为34.5×10^-6、70.71×10^-6，La/Yb，LREE/HREE，（La/Yb）_N 校正后的平均值分别为 11.32，8.13，7.67，δEu 校正后的平均值为 0.82，表明其与大陆岛弧相近，且 La-Th-Sc，Th-Sc-Zr/10和Th-Co-Zr/10等 3 个三角图显示其构造背景为大陆岛弧。因此，研究区东岳庙段物质来源于北东侧大巴山和东南侧江南古陆（雪峰古陆）。

关键词: 泥页岩, 稀土元素, 微量元素, 温暖湿润淡水沉积, 上地壳花岗岩, 大陆岛弧, 东岳庙段, 自流井组, 下侏罗统, 川东地区

Abstract: A set of dark shale is developed in Dongyuemiao member of Lower Jurassic Ziliujing Formation in eastern Sichuan Basin，which has great potential for shale gas exploration and development. By combining the macro tectonic background with the analysis of micro petrological characteristics，and using trace element（including rare earth elements）data，the sedimentary environment and material sources of the shale of Dongyuemiao member of Lower Jurassic Ziliujing Formation in eastern Sichuan Basin were analyzed and discussed. The results show that：（1）Gray shell limestone，gray siltstone，dark gray shell mudstone，gray black shale，and gray-to-dark gray mudstone were deposited from bottom to top in Dongyuemiao member of Lower Jurassic in eastern Sichuan Basin. （2）Rare earth elements of shale of Dongyuemiao member in the study area are characterized by enrichment of light rare earth elements，heavy rare earth elements loss. δCe is a negative anomaly，with an average Ce_anom value of -0.015，V（/ V+Ni）average value of 0.70，Sr/Cu average value of 2.43，Sr/Ba average value of 0.16，and（La/ Yb）_N average value of 1.32. The sedimentary environment of shale is relatively oxygen-poor and weakly reductive，and it is generally in a warm and humid climate with light water deposition，with fast deposition rate， which is conducive to the enrichment of organic matters.（3）The Zr/Sc-Th/Sc and La/Sc-Co/Th plots show that the sedimentary parent rock in the study area is granite. The values of Th/Sc，Th/Co，Th/Cr and La/Sc are 0.78， 0.65，0.14 and 2.14，respectively，all of which are close to the corresponding element ratios of the upper crust， indicating that the parent rock is mainly granite from the upper crust. The average mass fractions of corrected La and Ce elements are 34.5×10^-6 and 70.71×10^-6，respectively，and the average values of corrected La/Yb，LREE/ HREE，（La/Yb）_N are 11.32，8.13 and 7.67，respectively，and the average value of corrected δEu is 0.82，indicating that they are similar to those of continental island arc. The triangle diagram of La-Th-Sc，Th-Sc-Zr/10 and Th-Co-Zr/10 show that its tectonic background is a continental island arc. Therefore，the provenance of Dongyuemiao member in the study area comes from Daba Mountain in the northeast and Jiangnan ancient land（Xuefeng ancient land）in the southeast.

Key words: shale, rare earth element, trace element, warm and humid fresh-water deposit, upper crustal granite, continental island arc, Dongyuemiao member, Ziliujing Formation, Lower Jurassic, eastern Sichuan Basin

中图分类号:

TE121.3+1

邹连松, 徐文礼, 梁西文, 刘皓天, 周坤, 霍飞, 周林, 文华国. 川东地区下侏罗统自流井组东岳庙段泥页岩沉积特征及物质来源[J]. 岩性油气藏, 2024, 36(4): 122–135.

ZOU Liansong, XUWenli, LIANG Xiwen, LIU Haotian, ZHOU Kun, HOU Fei, ZHOU Lin, WEN Huaguo. Sedimentary characteristics and sources of shale of Dongyuemiao member of Lower Jurassic Ziliujing Formation in eastern Sichuan Basin[J]. Lithologic Reservoirs, 2024, 36(4): 122–135.

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川东地区下侏罗统自流井组东岳庙段泥页岩沉积特征及物质来源

Sedimentary characteristics and sources of shale of Dongyuemiao member of Lower Jurassic Ziliujing Formation in eastern Sichuan Basin

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