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Ordovician Granitoids and Silurian Mafic Dikes in the Western Kunlun Orogen, Northwest China: Implications for Evolution of the Proto‐Tethys
Author(s) -
ZHANG Qichao,
WU Zhenhan,
LI Shan,
LI Kan,
LIU Zhiwei,
ZHOU Qing
Publication year - 2019
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.13760
Subject(s) - mafic , geology , zircon , geochemistry , dike , pluton , partial melting , subduction , ordovician , crust , petrology , tectonics , paleontology
The western Kunlun orogen in the northwest Tibet Plateau is related to subduction and collision of Proto‐ and Paleo‐Tethys from early Paleozoic to early Mesozoic. This paper presents new LA‐ICPMS zircon U‐Pb ages and Lu‐Hf isotopes, whole‐rock major and trace elements, and Sr–Nd isotopes of two Ordovician granitoid plutons (466–455 Ma) and their Silurian mafic dikes (∼436 Ma) in the western Kunlun orogen. These granitoids show peraluminous high‐K calc‐alkaline characteristics, with ( 87 Sr/ 86 Sr) i value of 0.7129–0.7224, ε Nd (t) values of –9.3 to –7.0 and zircon ε Hf (t) values of –17.3 to –0.2, indicating that they were formed by partial melting of ancient lower‐crust (metaigneous rocks mixed with metasedimentary rocks) with some mantle materials in response to subduction of the Proto‐Tethyan Ocean and following collision. The Silurian mafic dikes were considered to have been derived from a low degree of partial melting of primary mafic magma. These mafic dikes show initial 87 Sr/ 86 Sr ratios of 0.7101–0.7152 and ε Nd (t ) values of –3.8 to –3.4 and zircon ε Hf ( t ) values of –8.8 to –4.9, indicating that they were derived from enriched mantle in response to post‐collisional slab break‐off. Combined with regional geology, our new data provide valuable insight into late evolution of the Proto‐Tethys.