西秦岭舒家坝地区泥盆纪舒家坝群碎屑锆石LA-ICP-MSU-Pb年龄:源区特征与形成时代  

Detrial zircon LA-ICP-MS UPb ages of the Devonian Shujiaba Group in Shujiaba area of the West Qinling tectonic zone: Constraints on material source and sedimentaryage

作　　者：王元元[1] 裴先治[1,2] 刘成军[1] 李瑞保[1,2] 李佐臣[1,2] 魏博[1] 任厚州 陈伟男[1] 刘图杰 胥晓春 

机构地区：[1]长安大学地球科学与资源学院,陕西西安710054 [2]西部矿产资源与地质工程教育部重点实验室,陕西西安710054

出　　处：《地质通报》2014年第7期1015-1027,共13页Geological Bulletin of China

基　　金：国家自然科学基金项目(批准号:41172186;40972136;40572121);教育部高等学校博士学科点专项科研基金项目(编号:20110205110004);中央高校基本科研业务费专项(编号:CHD2011TD020;2013G1271091;2013G1271092)

摘　　要：以西秦岭舒家坝地区泥盆纪舒家坝群碎屑岩为研究对象,进行碎屑锆石LA-ICP-MS U-Pb年龄研究,探讨其形成时代、物源组成和构造背景。所测样品最小锆石年龄组的年龄加权平均值为413Ma,代表了舒家坝群的沉积下限,结合前人研究的古生物资料将其形成时代限定为中泥盆世。所获碎屑锆石年龄可划分为4个谱段：震旦纪—古生代年龄谱段619～409Ma,峰值为445Ma;新元古代年龄谱段930～735Ma,峰值为849Ma;中元古代年龄谱段1760～1033Ma;新太古代—古元古代年龄谱段3095～2478Ma。综合研究认为,舒家坝群的物源具多元性,包括西秦岭北缘构造带、北祁连造山带东段和华北板块基底,其中北祁连造山带东段和西秦岭北缘构造带是舒家坝群沉积的主要物源区,且后者占主导地位。结合区域地质资料,根据其物源组成特征判断,舒家坝群形成于陆—陆或弧—陆碰撞后由挤压转换为伸展环境的局部裂陷盆地。Choosing the Shujiaba Group detrital rocks in Shujiaba area as the study object and using LA-ICP-MS zircon U-Pb isotope chronology, the authors studied the sedimentary age and material source of the Shujiaba Group. 413 Ma, the mean of the minimum ages group, indicates that the sedimentary age of Shujiaba Group should be the Middle Devonian. Four groups can be recognized from the zircon ages spectrum： Sinian-Early Paleozoic age group（619～409Ma）, with the peak value of 445Ma;Neoproterozoic age group（930～735Ma）, with the peak value of 849Ma; Mesoproterozoic age group（1760～1033Ma）; and Paleoproterozoic-Neoarchaen age group（3095～2478Ma）. The age group information indicates that the material sources were mainly derived from North Qilian orogenic belt,the northern margin of West Qinling tectonic zone and the basement of North China block, of which the North Qilian orogenic belt and the northern margin of West Qinling tectonic zone made the major contribution, with the last one playing the leading role. The material source features and regional geology suggest that the Shujiaba Group was formed in a rifted basin resulting from the transitional tectonic setting from syn-collision（compressional setting） to post-collision（extensional setting）.

关 键 词：碎屑锆石 舒家坝群 形成时代 物源 构造环境 西秦岭 

分 类 号：P534.44[天文地球—古生物学与地层学] P597.3[天文地球—地质学]