南华北地区及其北部邻区上石炭统-中二叠统高分辨率层序地层  

High-resolution Stratigraphy of Upper Carboniferous-Middle Permian in Southern North China and Its Northern Surroundings

作　　者：李杨 阮壮[1] 李中明[2] 于炳松[1] 宋南南 董果果 张栋[2] LI Yang;RUAN Zhuang;LI Zhongming;YU Bingsong;SONG Nannan;DONG Guoguo;ZHANG Dong(School of Earth Sciences and Resources,China University of Geosciences,Beijing100083,China;Henan Institute of Geological Survey,Zhengzhou,Henan450001,China)

机构地区：[1]中国地质大学(北京)地球科学与资源学院,北京100083 [2]河南省地质调查院,河南郑州450001

出　　处：《现代地质》2020年第4期718-731,共14页Geoscience

基　　金：河南省国土资源厅科技攻关项目“河南省平原区晚古生代页岩气层岩相古地理研究”(2015-1992-20);河南省重大科技专项项目“河南页岩气勘查开发及示范应用研究”(151100311000)。

摘　　要：南华北地区石炭系—二叠系烃源岩广泛发育,是未来页岩气勘探的重要目标;然而,其研究程度低,区域地质构造复杂,岩性地层对比关系不清。基于高分辨率层序地层学及沉积学的相关理论,以区内12口井的钻测井资料和两口井的岩心资料为依据,开展了南华北地区及北部邻区上石炭统—中二叠统层序地层划分。结果显示,研究区内太原组、山西组和下石盒子组属于一个不完整的超长期旋回,内部可划分为5个长期旋回和14个中期旋回。中期基准面旋回结构样式可分为3类:(1)以上升半旋回为主的不完全对称类型,多发育在近岸三角洲背景下;(2)以下降半旋回为主的不完全对称类型,多发育在深水的潮间-潮下/潟湖环境;(3)上升半旋回与下降半旋回近于相等的近完全-完全相等的对称类型,在三角洲和潮坪相浅水区域均有发育。从南北向与东西向层序地层年代格架剖面分析可以发现,研究区内不存在大型的或者区域性的沉积间断与不整合面,但研究区因后期构造作用,南部与北部产生“翘板式”转换抬升,局部出现剥蚀间断,形成与上、下地层假整合接触。Permo-Carboniferous source rocks in southern North China are widely developed and become an important target for shale-gas exploration.However,regional study on the Carboniferous-Permian sequences is still inadequate due to the complex structure and unclear stratigraphic correlation.Based on high-resolution stratigraphy,sedimentology,core-logging,and seismic data from twelve wells,we first establish the stratigraphic sequence of the region.The results show that the Taiyuan,Shanxi and Xiashihezi formations belong to an incomplete super-long cycle,which could be divided into five long-term cycles and 14 medium-term cycles.The medium-term base-level circle structure patterns can be divided into three types:A and B,incomplete symmetrical type dominated by(A)ascending hemicycle and(B)descending semicircular gyrus;C,nearly half ascending and half descending with the same type of symmetry.A-type patterns are mostly developed in the nearshore delta sedimentary environment,whilst B-type patterns are mostly developed in the intertidal to subtidal/lagoon environment.Meanwhile,C-type patterns are common in shallow-water(deltaic or tidal)environments.Geostatistical analysis of the stratigraphic sequences(from north to south and from east to west)has found no regional discontinuities or unconformities.Due to local late-tectonic influence,the seesaw-style uplift may have generated local discontinuities,which formed the pseudo-unconformity between the upper and lower parts of the sequence.

关 键 词：南华北地区 上石炭统—中二叠统 高分辨率层序地层 基准面旋回 

分 类 号：P534.4[天文地球—古生物学与地层学] P539.2[天文地球—地质学]