西秦岭造山带泥盆纪沉积地质学和动力沉积学：西秦岭北带泥盆纪前陆盆地的沉积特征及盆地格局  

SEDIMENTARY GEOLOGY AND DYNAMIC SEDIMENTOLOGY OF THE DEVONIAN STRATA IN THE WEST QINLING OROGENIC BELT:SEDIMENTARY CHARACTERISTICS AND FRAMEWORK OF THE DEVONIAN FORELAND BASIN IN THE NORTHERN BELT OF THE WEST QINLING OROGENIC BELT

作　　者：杜远生[1] 

机构地区：[1]中国地质大学

出　　处：《沉积与特提斯地质》1995年第4期47-62,共16页Sedimentary Geology and Tethyan Geology

摘　　要：秦岭造山带是横亘于华北、扬子两板块之间的巨型造山带，在中国古大陆地壳形成演化中占有十分重要的地位。作为连接造山带加里东一海百、印支阶段重要一环的泥盆系对恢复造山带沉积和构造演化意义重大。本文仅从西秦岭北带泥盆系地层和沉积学人手，探讨该区早海西期的盆地格局和构造特征。西秦岭北带泥盆系包括舒家坝群和大草滩群（包括红相和绿相两种类型），前者以临滨－陆棚－半深海背景沉积和风暴流、重力流事件沉积为特色；后者以辫状河和网状河（红相）和湖泊－水下冲积扇和深湖重力流（绿相）沉积为特征。沉积特征和充填序列都反映其形成于压性的前陆盆地背景下。该前陆盆地是由于北秦岭造山带的向南仰冲，在中秦岭微板块北缘形成的。The Qinling orogenic belt lying between the North China Plate and Yangtze Plate plays an important part in explaining the formation and evolution of palaeo continents in China.As an important link between the Caledonian and Hercynian tectonic stages,the De- vonian strata in the belt has all along been considered as the key bed to decipher the sedi- mentary and tectonic evolution in the study area.The present paper focuses on the early Hercynian basin framework and tectonic features based on stratigraphy and sedimentology of the Devonian strata in the northern belt of the West Qinling orogenic belt.The Devoni- an strata in this region consist of the Shujiaba and Dacaotan Groups (including two types: red facies and green facies).The former is characterized by the nearshore-shelf-bathyal background deposits,storm deposits and gravity flow deposits,while the latter by the braided and anastomosed deposits(red facies)and lake-subaquenous alluvial fan,deep-lake gravity flow deposits (green facies).These depositional characteristics and infilling se- quences indicate the existance of the foreland;which was formed on the northern margin of the central Qinling microplate due to the southward obduction of the northern Qinling oro- genic belt during early Hercynian stage.

关 键 词：秦岭造山带 泥盆系 前陆盆地 沉积地质学 

分 类 号：P512.2[天文地球—地质学]