|Table of Contents|

Geochronological Characteristics of Devonian Granitoids in Kelan Basin of Altay, Xinjiang, China and Their Geological Implications(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2019年第04期
Page:
414-430
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Geochronological Characteristics of Devonian Granitoids in Kelan Basin of Altay, Xinjiang, China and Their Geological Implications
Author(s):
ZHANG Zhong-li1;  YANG Cheng-dong2*;  ZHANG Bin1;  WANG Yong-qiang1;  LI Qiang2;  YANG Fu-quan2
(1. No. 706 Geological Team, Xinjiang Nonferrous Geoexploration Bureau, Altay 836500, Xinjiang, China; 2. MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037, China)
Keywords:
geochronology;  granite;  zircon U-Pb age;  Devonian;  magmatic intrusion;  Kelan Basin;  Altay;  Xinjiang
PACS:
P588.12+1; P597
DOI:
-
Abstract:
Granitic intrusions are widespread in and around Kelan Basin of Altay, Xinjiang, China. With the aim to provide a new basis for further study on the origin and evolution of Kelan Basin, the detailed petrologic and geochronological constraints on the granitoids in the southwestern and northeastern segments of Kelan Basin were presented. Lithologies of the samples include medium-fine-grained two-mica-bearing syenogranite, medium-coarse-grained two-mica monzonite granite, muscovite monzonite granite, and medium-coarse-grained tonalite. The LA-MC-ICP-MS zircon U-Pb dating yields the ages of(404.6±4.7),(386.7±4.8),(395.6±2.9)and(406.6±3.1)Ma, respectively, indicating that the intrusion occurs in Early-Middle Devonian. Combined with the references of the regional geochronology and tectonic setting, the granitoids in Kelan Basin are thought to have been emplaced during Ordovician, Devonian and Permian. The Devonian granitoid has the largest distribution, especially the age of 400 Ma represents the peak intrusive phase of Kelan Basin, which is consistent with that of the entire Altay. The age of Devonian granitoid is slightly later than that of Kangbutiebao Formation in Kelan Basin. The temporal and spatial relationships between the granitoids and volcanic rocks indicate that they are the products of the same magmatic event in a continental arc setting.

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Last Update: 2019-07-11