河南省太原组沉积时期岩相古地理特征  

Characteristics of Lithofacies Paleogeography of the Taiyuan Formation Sedimentary Period,Henan Province

作　　者：宋慧波[1] 胡斌[1] 张璐[1] 刘顺喜[1] 牛永斌[1] 

机构地区：[1]河南理工大学资源环境学院河南省生物遗迹与成矿过程重点实验室,河南焦作454003

出　　处：《沉积学报》2011年第5期876-888,共13页Acta Sedimentologica Sinica

基　　金：国家自然科学基金项目(批准号:40872001;41102002);国家高校博士点专项基金(编号:20094116110002);河南省科技计划项目(编号:092300410167);河南省生物遗迹与成矿过程重点实验室开放基金(编号:OTMP0904)资助

摘　　要：河南省早二叠世太原组沉积区位于华北盆地南部北秦岭褶皱带栾川—固始深断裂以北地区,当时的沉积盆地受华北地块西隆东倾的构造古地理控制,是晚古生代华北陆表海盆地或碳酸盐岩台地沉积的一部分,发育了一套以碳酸盐岩为主夹碎屑岩和煤为特色的陆表海沉积。太原组岩性以灰—深灰色薄—中厚层状生物屑灰岩为主,夹薄—中厚层状的泥岩、泥灰岩、细砂岩、粉砂岩及煤层,局部出现浅灰色厚层中一细粒砂岩、粗砂岩或灰白色石英砂岩,产有丰富的纺锤虫、牙形石、腕足、珊瑚、海百合、双壳类和植物化石等。在沉积序列上,自下而上分为三个岩性段,即①下部灰岩段,主要由4～5层灰岩组成;②中部碎屑岩段,主要由砂、泥岩组成,夹不稳定生物屑微晶灰岩1～3层;③上部灰岩段,含灰岩2～3层,局部可达4～5层。基于地层厚度、碳酸盐岩厚度和砂/泥比等值线的变化趋势分析以及遗迹化石、指相化石和沉积类型的组成与分布特征,可以划分出5种沉积相(潮坪相、潟湖相、障壁岛或砂坝相、局限台地相和开阔台地相)、12种沉积类型、3种沉积组合类型和3种岩相区,包括局限台地—潮坪泥晶灰岩、泥岩相区、开阔台地—潮坪—潟湖灰岩、碎屑岩相区、开阔台地—障壁岛—潮坪灰岩、碎屑岩相区。太原组沉积期的古地理特征表现为:海域分布广泛,海相灰岩几乎遍及全区;海陆边界已向南、向西扩至灵宝—洛宁—嵩县—方城—泌阳一线,该线以西为伏牛古陆,三门峡至济源一线以北为中条古陆,古地势呈现为北西高、南东低,西陡东缓,最大厚度沉积区位于东北部及东部的特点;海水自东和北东两个方向侵入,并自北西向南东方向退去。由于沉积区域内地形比较平缓,海水进退频繁,形成了一套受限陆表海的碳酸盐岩与滨岸潮坪含煤碎屑岩多次交互出现的沉积,在河�The sedimentary area of the Early Permian Taiyuan Formation in Henan Province is located in the south ofnorth China basin and to the north of Luanchuan-Gushi deep fault in the North Qingling fold belt,at that time,thissedimentary basin was controlled by the tectono-paleogeographic features of the west uplift in the North China platformblock.The Taiyuan Formation was a part of deposits of the North-China epicontinental sea or carbonate platform in the Late Paleozoic,and developed a set of deposits of the epicontinental sea characterized by the carbonate rocks intercalated some clastic rocks and coal.This section is mainly composed of gray,dark gray,thin-medium bedded bioclasticlimestones,intercalated with thin-medium bedded mudstone,micritic limestone,fine sandstone,siltstones and thincoals,locally appeared light gray thick beded moderate-fine grained sandstone,coarse sandstone or gray-white quartzsandstone,with very abundant body fossils,such as fusulinids,conodonts,brachiopods,corals,crinoids,bivalves andplants fossils and so on.According to the analysis of sedimentary sequence,the Taiyuan Formation can be divided in-to three units from bottom to top： the lower limestone unit,mainly containing 4 ～ 5 limestone layers;the middleclastic unit,dominated by sandstone and mudstone,intercalated with 1 ～ 3 layers of limestone,unstable bioclastic mi-crocrystalline limestone;the upper limestone unit,composed of 2 ～ 3 layers of limestone,locally,4 ～ 5 layers.Based on the isoline trend analysis including the thickness of the formation and carbonate rock and the ratio of sand tomudstone,along with the composition and distribution features of ichnofossils,facies fossils and sedimentary assem-blage types,5 sedimentary facies（tidal-flat,lagoon,barrier island or sand bar,restricted carbonate platform andopen carbonate platform facies）,12 kinds of sedimentary types,3 sedimentary assemblage types and 3 types of litho-facies areas as the micritic limestone and mudstone lithofacies area of restricted flatform-tidal flat

关 键 词：沉积相 岩相古地理 太原组 早二叠世 河南省 

分 类 号：P512.2[天文地球—地质学]