镇巴地区灯影组岩石微相研究与沉积环境分析

doi:10.11885/j.issn.1674-5086.2020.02.19.02

西南石油大学学报(自然科学版) ›› 2020, Vol. 42 ›› Issue (3): 31-42.DOI: 10.11885/j.issn.1674-5086.2020.02.19.02

镇巴地区灯影组岩石微相研究与沉积环境分析

侯明才^1,2, 何亮^1,2, 徐胜林^1,2, 汤智江^1,2

1. 成都理工大学沉积地质研究院, 四川成都 610059;
2. 油气藏地质及开发工程国家重点实验室·成都理工大学, 四川成都 610059

收稿日期:2020-02-19 出版日期:2020-06-10 发布日期:2020-06-10
通讯作者: 何亮,E-mail:1206055802@qq.com
作者简介:侯明才,1968年生,男,汉族,四川南部人,教授,博士生导师,主要从事大地构造沉积学、含油气盆地分析、层序岩相古地理学等领域的科研、教学工作。E-mail:houmc@cdut.edu.cn;何亮,1992年生,男,汉族,甘肃民勤人,硕士研究生,主要从事层序地层学与岩相古地理等方面的研究。E-mail:1206055802@qq.com;徐胜林,1981年生,男,汉族,安徽望江人,副教授,主要从事层序岩相古地理学与储层地质学等领域的教学、科研工作。E-mail:xusheng218@163.com;汤智江,1994年生,男,汉族,四川广安人,硕士研究生,主要从事沉积学、岩相古地理研究。E-mail:1099663589@qq.com
基金资助:
国家科技重大专项（2017ZX05008-005-009）

Analysis of Rock Types and Sedimentary Environment of Dengying Formation, Zhenba Area

HOU Mingcai^1,2, HE Liang^1,2, XU Shenglin^1,2, TANG Zhijiang^1,2

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan 610059, China

Received:2020-02-19 Online:2020-06-10 Published:2020-06-10

摘要/Abstract

摘要： 上扬子地区灯影组可以作为优质储层已经被油气勘探所证实。但是，由于灯影组储层的展布规律一直不清楚，制约了对灯影组的进一步勘探。基于镇巴地区鹿池灯影组剖面，开展了详细的岩石微相研究，结合碳、氧同位素和微量元素分析，深入探讨了镇巴地区灯影组的沉积环境。研究表明，镇巴地区震旦系灯影组岩石微相有：泥-粉晶云岩、残余砂屑云岩、叠层石云岩、凝块石云岩、微生物黏结砂屑云岩、泥质粉砂岩、泥质云岩和含云质硅质岩。研究区灯影组沉积环境为开阔碳酸盐岩台地，经历了两次海侵-海退旋回，灯一段-灯二段和灯三段灯四段分别为两个相对完整海侵-海退序列。相对于灯二段，灯四段海平面振荡更频繁，可能与拉张活动在灯四期更活跃有关。碳氧同位素和微量元素数据表明，灯影组的沉积古环境发生了较为剧烈的变化。整体而言，灯影期大致是一个海水盐度下降，温度上升，含氧量逐步增加的过程。

关键词: 岩石微相, 沉积环境, 灯影组, 震旦系, 镇巴地区

Abstract: As a high-quality reservoir of the lower assemblage, the Dengying Formation have been proved by the oil and gas exploration. However, the distribution of reservoir is not yet clear. Based on the outcrop of Dengying Formation at Luchi section, Zhenba Area, this paper carries out a detailed study of the sedimentary microfacies. Furthermore, combined with microscopic characteristics, the sedimentary characteristics and genesis of eight types of rocks are sorted out and explained. These rock types include micritic dolostones, residual dolarenite, stromatolite dolostones, thrombolite dolostones, microbe-bonded dolarenite, argillaceous siltstone, argillaceous dolostones and (dolomite-bearing) siliceous rock. The sedimentary environment of Dengying Formation in the study area is open carbonate platform, which has experienced two transgression-regressive cycles.The carbon and oxygen isotope and trace element data indicate that the sedimentary paleoenvironment during deposition of Dengying Formation changed dramatically. On the whole, the deposition period of the Dengying Formation is roughly featured with the decreasement of seawater salinity, increasement of seawater temperature and gradual increasement of oxygen content, but the environmental fluctuations may exist.

Key words: rock microfacies, sedimentary environment, Dengying Formation, Sinian System, Zhenba Area

中图分类号:

TE122

侯明才, 何亮, 徐胜林, 汤智江. 镇巴地区灯影组岩石微相研究与沉积环境分析[J]. 西南石油大学学报(自然科学版), 2020, 42(3): 31-42.

HOU Mingcai, HE Liang, XU Shenglin, TANG Zhijiang. Analysis of Rock Types and Sedimentary Environment of Dengying Formation, Zhenba Area[J]. 西南石油大学学报(自然科学版), 2020, 42(3): 31-42.

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镇巴地区灯影组岩石微相研究与沉积环境分析

Analysis of Rock Types and Sedimentary Environment of Dengying Formation, Zhenba Area

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