潜江凹陷潜三段-潜四上亚段沉积相研究 |
| |
引用本文: | 刘宇琦,李建明,刘云生,张广英. 潜江凹陷潜三段-潜四上亚段沉积相研究[J]. 石油天然气学报, 2009, 31(1): 171-173 |
| |
作者姓名: | 刘宇琦 李建明 刘云生 张广英 |
| |
作者单位: | [1]长江大学地球科学学院,油气资源与勘探技术教育部重点实验室,湖北荆州434023 [2]江汉油田分公司勘探开发研究院,湖北潜江830013 |
| |
摘 要: | 根据古地形、岩心观察、测井曲线等特征.认为潜江组发育三角洲、淡一半咸水湖、盐湖等沉积体系。潜江凹陷碎屑物来源比较单一.主要来自于西部及北部。以西部荆门物源为主,汉水、乐乡关及永隆河物源次之。总体具有北部单向远物源、西强东弱、继承性供给的特点。研究区总体上。自北西向南东方向,由三角洲沉积体系变为淡-半成水滨浅湖沉积体系.再变为盐湖沉积体系。潜江凹陷砂体主要呈北西方向展布是岩性油藏发育的有利区带。
|
关 键 词: | 潜江凹陷 潜江组 沉积微相 岩性油藏 |
Study on Sedimentary Facies of the Upper Members in Eq_3-Eq_4 of Qianjiang Depression |
| |
Abstract: | The features of ancient landform,core observation,logging curve showed that different types of sedimentary systems were developed in Qianjiang Formation of Qianjiang Depression,such as delta,freshwater-brackish lake,saline etc.The sources of depression clastic materials were unitary,and most of them came from the west and north.The provenance was mainly from Jingmen in the west,and then from Han River,Lexiangguan and Yonglong River.There is a distal single directional sedimentary source in the north of Qian... |
| |
Keywords: | Qianjiang Depression Qianjiang Formation sedimentary microfaices lithologic deposit |
本文献已被 CNKI 维普 等数据库收录! |
|