上扬子北缘震旦纪-早古生代沉积演化与储层分布特征
- 1、下载文档前请自行甄别文档内容的完整性,平台不提供额外的编辑、内容补充、找答案等附加服务。
- 2、"仅部分预览"的文档,不可在线预览部分如存在完整性等问题,可反馈申请退款(可完整预览的文档不适用该条件!)。
- 3、如文档侵犯您的权益,请联系客服反馈,我们会尽快为您处理(人工客服工作时间:9:00-18:30)。
上扬子北缘震旦纪-早古生代沉积演化与储层分布特征
余谦;牟传龙;张海全;谭钦银;许效松;闫剑飞
【期刊名称】《岩石学报》
【年(卷),期】2011(027)003
【摘要】The sedimentary evolution of the northern Upper Yangtze plate is affected by South Qinling structure on the north, Longmenshan structure on the west, and also long-term inherited uplift of Hannan paleocontinent on the north. In Sinian-Early Paleozoic with Qinling Sea on the north, Bayan Har Sea on the west, its sedimentary filling evolution is different from NE edge of Yangtze plate. On top of volcanic-sedimentary rock of Tiechuanshan Formation-Xixiang Formation and tillite of Nanhua System, mainly underwent carbonate platform in Sinian, shelf in Early-Middle Cambrian, carbonate platform and pericratonic uplift in Late Cambrian-Early Ordovician, platforms drowning in Middle Ordovician, and shelf deposition in Late Ordovician-Early Silurian. Some sets of regional source rock and favorable reservoir are formed in the sedimentary evolution. The reservoir mainly include algal reef-dolomite reservoir of Denigying Formation, oolitic limestone reservoir of Xiannvdong Formation, sand reservoir of Canglangpu Formation, and dolomite reservoir of Shilongdong Formation. The reservoir distributes widely. Although dominated by low porosity and low permeability overall, carbonatite reservoir in some areas develops corrosion and the permeability is favorable. The Dingying
Formation and Shilongdong Formation are the main reservoir and potential exploration target in northern Yangtze plate, in which oil and gas exploration potential is considerable.%上扬子北缘地层沉积演化既受北部南秦岭构造、西部龙门山构造、同时也受北部汉南古陆的长期继承性隆起影响.震旦纪-早古生代,其北部为秦岭洋、西部为巴颜喀拉洋,沉积充填演化序列有别于扬子地台东南边缘.在铁船山组-西乡组火山-沉积岩系和南华系冰碛岩之上,主要经历了震旦纪初始碳酸盐台地、早中寒武世陆棚、晚末寒武世-早奥陶世碳酸盐台地及克拉通边缘隆升、中晚奥陶世台地淹没、晚奥陶-早志留世滞留陆棚沉积等阶段.沉积演化过程中,上扬子北缘地区形成了多套区域性烃源岩,也形成了多套有利的储层,主要包括灯影组藻礁-白云岩储层、仙女洞组鲕粒灰岩储层、沦浪铺组砂体储层、石龙洞组白云岩储层.储层分布广泛,尽管总体以低孔低渗为主,但部分地区白云岩、灰岩储层溶蚀作用发育,储集性较好,灯影组与石龙洞组是主要的储层与潜在劫探目的层,具有较好的油气勘探潜力.
【总页数】9页(P672-680)
【作者】余谦;牟传龙;张海全;谭钦银;许效松;闫剑飞
【作者单位】成都地质矿产研究所,成都,610082;成都地质矿产研究所,成
都,610082;成都地质矿产研究所,成都,610082;成都地质矿产研究所,成都,610082;成都地质矿产研究所,成都,610082;成都地质矿产研究所,成都,610082
【正文语种】中文
【中图分类】P534.31;P534.4
【相关文献】
1.下扬子北缘前陆盆地构造演化及沉积特征 [J], 杜建波;何明喜;张艳霞;谢其锋;马
荣芳;张冬梅
2.晚三叠世中扬子北缘前陆盆地层序地层特征及沉积演化 [J], 陈留勤;段凯波;霍荣;胡水清
3.扬子地块西北缘后龙门山南华纪-早古生代沉积地层特征及其形成环境 [J], 李佐臣;王学良;裴先治;刘战庆;李瑞保;丁仨平;张晓飞;陈国超;刘智刚;陈有炘
4.汉南—川东北灯影组古地理演化:晚震旦世扬子西北缘拉张背景的沉积学证据 [J], YANG RuiQing;YANG FengLi;ZHOU XiaoFeng;ZHOU Zhi
5.扬子板块东北缘的随县-应山地区早古生代沉积盆地演化 [J], 杨振强;杨德骊;蒋德和
因版权原因,仅展示原文概要,查看原文内容请购买。