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阿尔金喀腊大湾地区卓阿布拉克组沉积岩系年代及其地质意义——来自碎屑锆石LA-ICP-MS U-Pb年龄的证据

陈安东 陈柏林 王永 孟令通 何江涛 韩梅梅 王斌

地质通报2018,Vol.37Issue(5):776-789,14.
地质通报2018,Vol.37Issue(5):776-789,14.

阿尔金喀腊大湾地区卓阿布拉克组沉积岩系年代及其地质意义——来自碎屑锆石LA-ICP-MS U-Pb年龄的证据

Geochronology of the sedimentary series from Zhuo'abulake Formation in Kaladawan area of Altun and its geological significance: LA-ICP-MS U-Pb age evidence of detrital zircons

陈安东 1陈柏林 1王永 1孟令通 2何江涛 3韩梅梅 1王斌3

作者信息

  • 1. 中国地质科学院地质力学研究所,北京100081
  • 2. 中国科学院地质与地球物理研究所,北京100029
  • 3. 中国地质大学(北京)地球科学与资源学院,北京100083
  • 折叠

摘要

Abstract

Choosing the conglomerate from the sedimentary series of Zhuo'abulake Formation in Kaladawan area as the study object and using LA-ICP-MS zircon U-Pb isotope chronology,the authors studied the sedimentary age,material source and tectonic setring of the sedimentary series.Some results were obtained:① The age spectra of detrital zircon can be evidently divided into two groups:522~427Ma and 638 ~ 1766Ma,with other two old ages 2450Ma and 3394Ma.② The youngest age of detrital zircons is 427±4Ma,suggesting that the formation of the conglomerate was later than 427Ma,and hence the formation age of the strata may be constrained from Late Silurian to Early Devonian (427~410Ma);Zhuo'abulake Formation should be divided into more units since it consists of materials from Late Cambrian to Early Devonian.② The peak value of the age spectrum is 456Ma,indicating that there existed a magmatic event during this period.The 522~432Ma age data possess the largest proportion and account for about 81% of the total data,showing that the magmatic rocks that were formed in early Paleozoic,especially from late Cambrian to Ordovician constituted the most important source of the conglomerate.The compositional ages suggest a sedimentary response to the orogenic erosion of a series of igneous rocks caused by the southward subduction and collision of Dunhuang massif in early Paleozoic period.③ Combining the recent research on North Qilian orogenic belt and the study of the detrital zircons in Kaladawan area,the authors consider that sedimentary series of Zhuo'abulake Formation in Kaladawan area and the Tianzhu Formation and Lujiaogou Formation in North Qilian have similar ages and material sources,and they may be the products of continental collision or arc-continent collision after North Qilian—North Altun limited ocean closure.

关键词

阿尔金/喀腊大湾地区/碎屑锆石/LA-ICP-MS锆石U-Pb定年/物源

Key words

Altun/Kaladawan area/detrital zircon/LA-ICP-MS zircon U-Pb dating/material source

分类

天文与地球科学

引用本文复制引用

陈安东,陈柏林,王永,孟令通,何江涛,韩梅梅,王斌..阿尔金喀腊大湾地区卓阿布拉克组沉积岩系年代及其地质意义——来自碎屑锆石LA-ICP-MS U-Pb年龄的证据[J].地质通报,2018,37(5):776-789,14.

基金项目

国家科技支撑计划重点项目专题《阿尔金成矿带多元信息成矿预测与找矿示范》(编号:2011BAB06B08-04) (编号:2011BAB06B08-04)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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