Global Geology 2017, 20(3) 153-163 DOI:   10.3969/j.issn.1673-9736.2017.03.03  ISSN: 1673-9736 CN: 22-1371/P

Current Issue | Archive | Search                                                            [Print]   [Close]
Articles
Information and Service
This Article
Supporting info
PDF(1271KB)
[HTML]
Reference
Service and feedback
Email this article to a colleague
Add to Bookshelf
Add to Citation Manager
Cite This Article
Email Alert
Keywords
Zhalaxiageyong
trachydacite
geochemistry
Zircon U-Pb age
Hf isotope
Authors
ZHANG Junyi
LI Bile
ZHAO Guoquan
NING Chuanqi
SUN Jing
WANG Guozhi
PubMed
Article by Zhang J
Article by Li B
Article by Zhao G
Article by Ning C
Article by Sun J
Article by Wang G

Geochemistry, U-Pb, Hf isotopic characteristics and geological significance of Zhalaxiageyong trachydacite in Tuotuohe area, Qinghai

ZHANG Junyi1, LI Bile1, ZHAO Guoquan2, NING Chuanqi1, SUN Jing1, WANG Guozhi1

1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Geological Team 7 of Qinghai Provincial Nonferrous Metal and Geological Exploration Bureau, Xining 810000, China

Abstract��

The Zhalaxiageyong lead-zinc-copper polymetallic deposit is a typical porphyry deposit of the Tuotuohe area. Whole-rock geochemical analyses, Zircon U-Pb dating and Hf isotope analysis are undertaken for the ore host trachydacite with the aim of constraining its petrogenesis, magma source and regional tectonic setting. LA-ICP-MS zircon U-Pb dating indicates that the trachydacite was formed in 32.68±0.50 Ma (MSWD=1.6), i.e., Oligocene. The trachydacite is rich in potassium and poor in Mg#(5.10-9.70), belonging to the peraluminous shoshonite series. The rocks are enriched in LILE (large ion lithophile elements) Rb, Ba, K and LREE, depleted in HFSE (high field strength elements) Nb, Ta, P, Ti, with high Sr and low Y and Yb, having the characteristics of the C type adakite. It is calculated that the initial εHf(t) of the zircons range from -0.92 to 2.07 and their two-stage Hf model ages TDM2 range from 978 Ma to 1 169 Ma. The magma source should be mainly the partially melt mafic rocks of the thickened Middle Neoproterozoic lower crust of the Northern Qiangtang massif with the addition of ancient aluminosilica material in the melting process. The rocks formed in the tectonic setting of delamination of lithosphere and extension of the thickened crust. During the period of 40-32 Ma, large-scale potassium rich alkaline magmatism occurred in this area. The porphyry metallogenesis is related to the magmatic activities in this period.

Keywords�� Zhalaxiageyong   trachydacite   geochemistry   Zircon U-Pb age   Hf isotope  
Received 2017-06-09 Revised 2017-07-03 Online:  
DOI: 10.3969/j.issn.1673-9736.2017.03.03
Fund:Supported by Project of China Geological Survey (No.12120114080901)
Corresponding Authors:
Email:
About author:

References��
Similar articles
1��YIN Yue, WANG Li, SUN Xia, JIANG Hefang, LI Liang.U-Pb geochronology, geochemistry and tectonic implications ofdiorite from Nangnimsan of Mehe in northern Da Hinggan Mountains[J]. Global Geology, 2017,20(4): 217-228
2��WANG Yang, SUN Fengyue, GAO Hongchang, HE Shuyue, QIAN Ye, XU Chenghan.Geochronology and geochemistry of Hutouya monzonitic granite of Qimantage, Qinghai[J]. Global Geology, 2017,20(4): 208-216

Copyright by Global Geology