Composition of the Fukeshan magmatic arc in the northern Great Xing’an Range: Constraints on the southward subduction of the Mongol-Okhotsk oceanic plate

doi:10.13745/j.esf.sf.2021.7.14

Abstract

Abstract:

The Fukeshan magmatic arc extends north-east in Fukeshan-Gulianhe area, northern Great Xing’an Range. Its material composition, formation age and spatial distribution pattern are very important for studying the Late Triassic tectonic evolution of the Mongol-Okhotsk ocean. In this paper, the petrology, geochemistry and zircon U-Pb dating of gabbro, diorite and granodiorite from the Fukeshan magmatic arc are reported, aiming to furthering our understanding of the tectonic setting of the northern Great Xing’an Range during the Late Triassic. LA-ICP-MS zircon U-Pb dating yielded the crystallization ages of (205.7±2.2) Ma and (203.2±2.5) Ma for gabbro and granodiorite, respectively, which correspond to the tectonic-magmatic event in the Late Triassic. Petrological and geochemical study indicate that the gabbro and diorite belong to tholeiite and calc-alkaline transition series rocks with high Na, Al, Ca, Mg and Mg^# contents and low Ti contents. They are enriched in large ion lithophile elements (LIFE) and light rare earth elements (LREE). The granodiorite belongs to calc-alkaline transition series rocks with high Si, Na and Al contents and low Mg contents. The rock has low content of Y and Yb, with no obvious negative Eu anomaly and belongs to O-type adakite. The Fukeshan magmatic arc has a distribution pattern from north to south, and the corresponding lithologic variation indicates the Mongol-Okhotsk ocean has a polarity of southward subduction.

Key words: northern Great Xing’an Range, Fukeshan magmatic arc, Late Triassic, Mongol-Okhotsk ocean, southward subduction

CLC Number:

P581
P597

LI Wenlong, YANG Xiaoping, QIAN Cheng, LI Chenglu, LÜ Mingqi, CHENG Zhaoxun, WANG Lijia. Composition of the Fukeshan magmatic arc in the northern Great Xing’an Range: Constraints on the southward subduction of the Mongol-Okhotsk oceanic plate[J]. Earth Science Frontiers, 2022, 29(2): 146-163.

Figures/Tables 13

Fig.1 Geological sketch maps of the Fukeshan area. a modified after [1]; b modified after [2].

Fig.2 Typical field rock outcrops and photomicrographs of Late Triassic intrusive rocks of Fukeshan area

Fig.3 Cathodeluminescence (CL) images of analyzed zircon (PM4LT2) from Late Triassic gabbro of Fukeshan area

Table 1 Zircon U-Pb data and age (PM4LT2) of Late Triassic gabbro in Fukeshan area

Table 2 Major and trace element contents of the tonalite and the diorite

Fig.4 U-Pb concordia diagrams for volcanic rocks from Late Triassic intrusive rocks of Fukeshan area

Fig.5 Cathodeluminescence (CL) images of analyzed zircon (PM12LT56) from Late Triassic granodiorite of Fukeshan area

Table 3 Major element, trace element and rare element compositions of Late Triassic intrusive rocks of Fukeshan area

Fig.6 Major element diagrams for volcanic rocks from Late Triassic intrusive rocks of Fukeshan area. Modified after [39-42].

Fig.7 (a) Chondrite-normalized rare earth element patterns (data from [43]) and (b) primitive mantle-normalized trace element spider diagrams (data from [44]) for Late Triassic intrusive rocks of Fukeshan area

Fig.8 La/Sm-Ba/Th (a) and Ba/La-Th/Yb (b) diagrams for Late Triassic intrusive rocks of Fukeshan area. Modified after 60.

Fig.9 (a) Sm/Yb-Sm (modified after [61-63]) and (b) La/Yb-Zr/Nb (modified after [64]) diagrams for Late Triassic intrusive rocks of Fukeshan area

Fig.10 (a) Sr/Y-Y (modified after [77]) and (b) (La/Yb)N-YbN (modified after [78]) for Late-Triassic intrusive rocks of Fukeshan area

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