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内蒙二连盆地赛汉塔拉凹陷下白垩统层序地层及有利成藏条件
引用本文:尹志军,田世清,杨志彬,姜燕,高丽,涂先俊,闫耀成,张凤红.内蒙二连盆地赛汉塔拉凹陷下白垩统层序地层及有利成藏条件[J].古地理学报,2009,11(3):330-337.
作者姓名:尹志军  田世清  杨志彬  姜燕  高丽  涂先俊  闫耀成  张凤红
作者单位:1.中国石油大学(北京)油气资源与探测国家重点实验室,北京102249;2.中国石油华北油田采油四厂地质研究所, 河北廊坊 065000;3.中国石油华北油田分公司二连地质研究所, 内蒙古锡林浩特 026017;4.中国石油华北油田分公司二连工程技术研究所,内蒙古锡林浩特 026017;5.中国石油大港油田分公司勘探开发研究院,天津300280
基金项目:教育部科学技术研究重大项目,国家自然科学基金重点项目 
摘    要:赛汉塔拉凹陷是二连盆地主要的油气富集凹陷之一,面积2300 km2〖KG-*2〗,探明石油地质储量1458万吨。论文应用层序地层学的基本理论,根据钻井和三维地震资料,在下白垩统中识别出5个层序界面,以此将该套地层划分为4个三级层序和12个体系域,建立了赛汉塔拉凹陷下白垩统层序地层格架。通过层序内部沉积体系及其演化的研究,对层序格架内的烃源岩条件、储集层条件等成藏要素进行了综合分析,确定了3套生储盖组合。综合分析表明,阿尔善组中下部、腾一段中部的近岸水下扇和浊积扇砂体,垂向上与烃源岩直接连通,可形成有效的生储盖组合,在凹陷生油中心附近易形成有效的岩性圈闭,成为凹陷最有利的油气聚集带,是下一步的重点勘探目标。

关 键 词:二连盆地  赛汉塔拉凹陷  下白垩统  层序地层  烃源岩  成藏条件

Sequence stratigraphy and beneficial hydrocarbon accumulation conditions of the Lower Cretaceous in Saihantala Sag,Erlian Basin,Inner Mongolia
Yin Zhijun,Tian Shiqing,Yang Zhibin,Jiang Yan,Gao Li,Tu Xianjun,Yan Yaocheng,Zhang Fenghong.Sequence stratigraphy and beneficial hydrocarbon accumulation conditions of the Lower Cretaceous in Saihantala Sag,Erlian Basin,Inner Mongolia[J].Journal of Palaeogeography,2009,11(3):330-337.
Authors:Yin Zhijun  Tian Shiqing  Yang Zhibin  Jiang Yan  Gao Li  Tu Xianjun  Yan Yaocheng  Zhang Fenghong
Abstract:The Saihantala Sag is one of the main hydrocarbon enrichment sags in Erlian Basin, with an area of 2300 km2 and proved geological reserves of 14580 000 tons. According to the basic theories of sequence stratigraphy, 5 sequence stratigraphic boundaries were recognized by seismic profile and drilling data, and as a result,the Lower Cretaceous of Saihantala Sag was classified into 4 third order sequences. The systems tracts were subdivided with first flooding surfaces and maximum flooding surfaces within each stratigraphic sequence and thus the sequence stratigraphic framework was established for the Lower Cretaceous of Saihantala Sag. Reservoir forming factors in different sequences, such as hydrocarbon source and reservoir condition,and so on,were comprehensively analyzed by studies of depositional systems and their evolution, and 3 sets of source reservoir cap rock assemblages were established in the Lower Cretaceous of Saihantala Sag. The sandbodies of sublacustrine fan and turbidite fan of the Lower Middle Aershan Formation and middle part of Member 1 of the Tenggeer Formation, which were connected with source rocks in vertical direction,are able to form effective lithologic traps around the oil generating center of Saihantala Sag. Thus they are the most favourable hydrocarbon accumulation zones and the main exploration targets of the Saihantala Sag. 
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