|
|||||
|
|
| 深水块状砂岩沉积特征及其成因机制探讨:以鄂尔多斯盆地东南缘上三叠统长6油层组为例 | |
| 引用本文： | 袁珍,李文厚,范萌萌,冯娟萍,郭懿萱. 深水块状砂岩沉积特征及其成因机制探讨:以鄂尔多斯盆地东南缘上三叠统长6油层组为例[J]. 地质科技情报, 2011, 30(4): 43-49 |
| 作者姓名： | 袁珍 李文厚 范萌萌 冯娟萍 郭懿萱 |
| 作者单位： | 1. 西北大学地质学系,西安 710069;西北大学大陆动力学国家重点实验室,西安 710069;西安石油大学油气资源学院,西安 710065 2. 西安科技大学地质与环境学院,西安,710054 3. 西北大学地质学系,西安,710069 |
| 基金项目： | 陕西省教育厅专项科研计划项目(09JK567) |
| 摘 要： | 近几年对鄂尔多斯盆地东南部延长组的石油勘探取得了重要突破,发现了多口达工业油流的油井.盆地东南部紧邻晚三叠世鄂尔多斯盆地湖盆沉积中心,在湖退背景下全盆广泛发育长6厚层砂体,目前已成为油气勘探的主要目标.依据岩心、露头观察等识别出长6沉积类型具有重力流沉积的特征,并认为盆地东南部长6沉积期广泛发育的深水块状砂岩属于受东北... |
| 关 键 词： | 鄂尔多斯盆地东南部 深水砂岩 长6油层组 重力流沉积 砂质碎屑流 滑塌 浊流 |
Genetic Mechanism and Sedimentary Features of Deep Water MassiveSandstone:A Case Study of the Upper Triassic Sandstones of Chang 6 Formation in the Southeast of Ordos Basin |
|
| YUAN Zhen , LI Wen-hou , FAN Meng-meng , FENG Juan-ping , GUO Yi-xuan. Genetic Mechanism and Sedimentary Features of Deep Water MassiveSandstone:A Case Study of the Upper Triassic Sandstones of Chang 6 Formation in the Southeast of Ordos Basin[J]. Geological Science and Technology Information, 2011, 30(4): 43-49 | |
| Authors: | YUAN Zhen LI Wen-hou FAN Meng-meng FENG Juan-ping GUO Yi-xuan |
| Affiliation: | YUAN Zhen1a,1b,2,LI Wen-hou1a,FAN Meng-meng3,FENG Juan-ping3,GUO Yi-xuan1a |
| Abstract: | Recently a major breakthrough has been made in the petroleum exploration in southeast of Ordos Basin and many commercial oil wells have been found in this area.The southeast area of the basin is close to sedimentation center of Triassic Ordos lake basin.The Chang 6 thick layer sandstone is widely developed under the background of lake regression and thus becomes the main target of oil exploration.Based on the large number of the core data and field observations,the sediment of gravity flows was identified f... |
| Keywords: | southeast of Ordos Basin deep water sand Chang 6 oil-bearing formation sediment of gravity flow sandy debris flow slump turbidity flow |
| 本文献已被 CNKI 万方数据 等数据库收录！ | |