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阿尔金造山带帕夏拉依档岩体锆石U-Pb年代学、地球化学特征及地质意义

张若愚 曾忠诚 朱伟鹏 陈宁 赵江林 李琦 王秦伟 饶静文

地质论评2016,Vol.62Issue(5):1283-1299,17.
地质论评2016,Vol.62Issue(5):1283-1299,17.DOI:10.16509/j.georeview.2016.05.013

阿尔金造山带帕夏拉依档岩体锆石U-Pb年代学、地球化学特征及地质意义

LA-ICP-MS Zircon U-Pb Dating,Geochemical Features and Their Geological Implications of Paxialayidang Plutons on the Southern Margin of Altyn Tagh

张若愚 1曾忠诚 1朱伟鹏 2陈宁 1赵江林 1李琦 1王秦伟 1饶静文1

作者信息

  • 1. 陕西省地质调查中心,西安,710068
  • 2. 太原理工大学矿业工程学院,太原,030024
  • 折叠

摘要

Abstract

The Paxialayidang plutons are located from the Paxialayidang ditch on South Altyn Tagh.The granitic rocks are mainly composed of monzonitic and porphyritic monzonitic.The U-Pb dating of zircons from the Paxialayidang plutons using LA-ICP-MS yields a group age of 460.1 ±3.9Ma ,indicating the crystallized-age of the plutons in Middle—Late Ordovician epoch.The geochemical analysis shows that major element characterized by high SiO2(72.08% ~72.27%),Al2O3 (14.10% ~14.79%),A/CNK =1.06 ~1.18 and K2O(5.55% ~6.33%)contents;low TiO2(0.19%~0.23%),MgO(0.22%~0.28%)and TFeO(1.48%~1.79%)contents, which suggest that syenogranite belong to the typical high-K calc-alkaline series with weakly peraluminous.In addition,they are enriched in total REE contents (165.58 ×10 -6 ~229.86 ×10 -6).The samples are enriched in LREE (light rare earth elements)and depleted in HREE (heavyrare earth elements)with Eu anomalies (δEu=0.1 1 ~0.17 ).The chondrite normalized REE pattern curve shows right-sloping type.The syenogranitees are riched in large ion lithophile elements of Rb,Th,K,U and depleted in high field strength elements of Ba,Sr,Ti and Rb/Sr value (9.05 ~12.57 ),with the characteristics of S-type granite,combining with the diagrams for discriminating compositions of original rocks,indicate the rock is forned by the partial melting of meta pelitic sedimentary rock from lower crust. Combined with the dataes of regional geological characteristics, the Paxialayidang plutons were formed in the transitional tectonic setting from the compressional to extensional segimes, belonging to the post-collisional granites.It shows that Altyn Tagh orogenic belt between blocks on both sides of Azhong Block with Qaidam Block suggests that it entered into transformation period from compression to extension during Middle—Late Ordovician epoch.

关键词

阿尔金山南缘/帕夏拉依档岩体/锆石U-Pb年代学/二长花岗岩/岩石成因

Key words

The South Altyn Tagh/Paxialayidang plutons/LA-ICP-MS zircon U-Pb dating/adamellite/petrogenesis

引用本文复制引用

张若愚,曾忠诚,朱伟鹏,陈宁,赵江林,李琦,王秦伟,饶静文..阿尔金造山带帕夏拉依档岩体锆石U-Pb年代学、地球化学特征及地质意义[J].地质论评,2016,62(5):1283-1299,17.

基金项目

本文为中国地质调查局项目(编号12120114081901、1212011120533)的成果。 ()

地质论评

OA北大核心CSCDCSTPCD

0371-5736

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