引用本文:李璟, 傅强, 邓秀琴, 黄健玲, 李祥同.鄂尔多斯盆地华池-庆阳地区延长组长62-63沉积微相研究[J].沉积与特提斯地质,2018,38(4):68-75.[点击复制]
[点击复制]
【打印本页】 【在线阅读全文】【下载PDF全文】 查看/发表评论下载PDF阅读器关闭

←前一篇|后一篇→

过刊浏览    高级检索

本文已被:浏览 240次   下载 146 本文二维码信息
码上扫一扫!
鄂尔多斯盆地华池-庆阳地区延长组长62-63沉积微相研究
李璟,傅强,邓秀琴,黄健玲,李祥同
0
(1. 同济大学海洋地质国家重点实验室, 上海 200092;
2. 中国石油长庆油田勘探开发研究院, 陕西 西安 710018;
3. 中国石化胜利油田分公司 东胜公司, 山东 东营 257001)
摘要:
为了更精准地研究鄂尔多斯盆地西南部华庆地区上三叠统延长组长62-63油层组储层特征,运用岩心照片、测井数据、粒度分析、录井数据等资料,对延长组长62-63油层组的岩性、碎屑颗粒、构造、测井响应、生物标志以及接触关系进行了分析研究。分析了长6油层组沉积微相特征,识别出该沉积时期半深湖-深湖亚相和三角洲前缘亚相两类沉积亚相,半深湖泥、浊积岩、砂质碎屑流砂体、水下分流河道、分流间湾和席状砂6类沉积微相,并分析华庆地区延长组长62-63期沉积相发育演化过程。沉积微相精细化描述揭示了华庆地区延长组6段油层组沉积环境,为精细化勘探开发提供地质依据。
关键词:  鄂尔多斯盆地  华庆地区  沉积微相  精细化  延长组
DOI:
附件
投稿时间:2018-05-13修订日期:2018-08-01
基金项目:国家科技重大专项(2016ZX05050)和(2017ZX050001002)资助
Sedimentary microfacies in the Chang-62 to Chang-63 oil reservoirs of the Upper Triassic Yanchang Formation in the Huachi-Qingyang region, Ordos Basin
LI Jing, Fu Qiang, DENG Xiu-qin, HUANG Jian-ling, LI Xiang-tong
(1. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
2. Research Institute of Petroleum Exploration and Development, Changqing Oil Field Company, CNPC, Xi'an 710018, Shaanxi, China;
3. Dongsheng Company Shengli Oilfield of SINOPEC, Dongying 257001, Shandong, China)
Abstract:
A detailed study is conducted, on the basis of core examination, grain-size analysis and well logs, to the lithology, grain size, sedimentary structure, well logging response, biomarker and contact relation of the Chang-62 to Chang-63 oil reservoirs of the Yanchang Formation in the Huachi-Qingyang region, Ordos Basin. The sedimentary facies in the study area may be classified into two sedimentary subfacies including the semi-deep lake to deep lake and delta front subfacies, and six sedimentary microfacies including the semi-deep lake mud, turbidite, sandy debris flow, subaqueous distributary channel, interdistributary bay and sheet sand microfacies. During the deposition of the Chang-63 oil reservoirs of the Upper Triassic Yanchang Formation, the shallow-lake delta front deposits were well developed in the semi-deep to deep lake sedimentary environments in the northeastern and southwestern parts of the study area, where the sandy debris flow deposits may provide excellent sites for the oil-gas accumulation in the deep lake area. The results of research in this study may be significant to the exploration and development of the Chang-6 oil reservoirs as the key exploration horizons of the Upper Triassic Yanchang Formation in the Huachi-Qingyang region.
Key words:  Ordos Basin  Huachi-Qingyang region  sedimentary microfacies  refinement  Upper Triassic Yanchang Formation

用微信扫一扫

用微信扫一扫