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Permian Tectonic Evolution in the Middle Part of Central Asian Orogenic Belt: Evidence from Newly Identified Volcanic Rocks in the Bilutu Area, Inner Mongolia
Author(s) -
WANG Shijie,
LIU Yang,
DONG Xiaojie,
XU Zhongyuan,
WANG Wenlong,
LI Shichao,
SHI Qiang,
CUI Weilong
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 - 10.1111/1755-6724.14361
Subject(s) - geology , dacite , zircon , andesite , geochemistry , partial melting , basalt , volcanic rock , basaltic andesite , subduction , mantle (geology) , fractional crystallization (geology) , continental arc , crust , continental crust , petrology , tectonics , volcano , paleontology
In this study, zircon U‐Pb ages, geochemical and Lu‐Hf isotopic data are presented for the newly identified volcanic rocks which were considered as Bainaimiao group in Bainaimiao Arc Belt (BAB), Inner Mongolia, which could provide important constraints on the evolution of the northern part of North China Block (NCB) and BAB. Basalt to basaltic andesite and andesite to dacite were collected from two sections, which showed eruption ages of 278.2±4.1 Ma and 258.3±3.0 Ma respectively. All samples are characterized by high abundances in Al 2 O 3 , LREEs, and LILEs, but depleted in HFSEs. Together with high Mg # ratios and low K/tholeiite to calc‐alkaline series, these features indicated that basalt to andesite was likely derived from relatively low degree partial melting of the subduction‐fluid related mantle in the spinel phase. And dacite was mainly from the partial melting of crust, then affected by mantle. All samples barely went through fractional crystallization process with the slight Eu anomaly. Compared with the contemporary basalt in NCB, rocks in BAB have a complex composition of zircon and a more positive ε Hf ( t ) value (–6.6–6.4), indicating that they had different magma sources of rocks. Though with different basements, NCB and BAB have become an integrated whole before 278 Ma. Therefore, it could be concluded that NCB and BAB belonged to the active continental margin and the PAO had not closed yet until late Permian and then it disappeared gradually and the CAOB developed into a condition of syn‐post collision.