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Geochronology and tectonic settings of Late Jurassic – Early Cretaceous intrusive rocks in the Ulanhot region, central and southern Da Xingan Range

Published online by Cambridge University Press:  24 June 2016

CHANGFENG LIU ,
ZHIGUANG ZHOU ,
YONGJU TANG ,
CHEN WU ,
HONGYING LI ,
YAN ZHU ,
TIAN JIANG ,
WENCAN LIU  and
BAOYING YE
CHANGFENG LIU*
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
ZHIGUANG ZHOU
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
YONGJU TANG
Affiliation:
China Geological Exploration Institute of Shandong Zhengyuan, Jinan 250101, China
CHEN WU
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
HONGYING LI
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
YAN ZHU
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
TIAN JIANG
Affiliation:
College of Zijin Mining, FuZhou University, Fuzhou 350108, China
WENCAN LIU
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
BAOYING YE
Affiliation:
School of Earth Science and Resources, China University of Geosciences (Beijing), Beijing 100083
*
†Author for correspondence: nose010@sohu.com
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Abstract

Zircon U–Pb dating and whole-rock geochemical analysis have been performed on Late Jurassic – Early Cretaceous intrusive rocks of the Ulanhot area, NE China, with the aim of constraining the tectonic evolution of the central and southern Da Xingan Range. Zircon U–Pb dating indicates that Late Jurassic – Early Cretaceous magmatic events experienced four stages at: c. 155 Ma; c. 144 Ma; 135–130 Ma; and c. 126 Ma. The c. 155 Ma magmatic event consists of quartz diorite and granite-porphyryp with the geochemical characteristic of high Sr and Sr/Y or high A/CNK (1.38), implying the primary magma was derived from partial melting of a thickened lower crust which induced the closure of the Mongol–Okhotsk Ocean. The c. 144 Ma magmatic event consists of quartz monzodiorite with the geochemical characteristics of alkaline series, and indicates the delamination of a thickened crust. The 135–130 Ma magmatic event consists of syenogranite and granite-porphyry with characteristics of both I-type and A-type granites, which induced both the subduction of the Palaeo-Pacific oceanic plate and the post-orogenic extension of the Mongol–Okhotsk Orogenic Belt. The c. 126 Ma magmatic event consisted of highly fractionated I-type biotite granite and alkaline series gabbro, marking the end of the Mongol–Okhotsk Orogen, and implying that the study area was controlled by the circum-Pacific tectonic system during this stage.

Keywords

Late Jurassic – early Cretaceousgabbro and granitic rocksgeochronologygeochemistrycentral and southern Da Xingan Range
Type
Original Articles
Information
Geological Magazine , Volume 154 , Issue 5 , September 2017 , pp. 923 - 945
Copyright
Copyright © Cambridge University Press 2016 

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