Whole-rock geochemistry and Sr-Nd-Pb isotope systematics of the Late Carboniferous volcanic rocks of the Awulale metallogenic belt in the western Tianshan Mountains (NW China): Petrogenesis and geodynamical implications

被引:40
|
作者
Ge, Songsheng [1 ,2 ]
Zhai, Mingguo [1 ]
Safonova, Inna [3 ,4 ]
Li, Dapeng [5 ]
Zhu, Xiyan [1 ]
Zuo, Pengfei [6 ]
Shan, Houxiang [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Inst Geol & Mineral SB RAS, Novosibirsk 630090, Russia
[4] Novosibirsk State Univ, Novosibirsk 630090, Russia
[5] Shandong Geol Sci Inst, Shandong Key Lab Geol Proc & Resource Utilizat Me, Key Lab Gold Mineralizat Proc & Resources Utiliza, Minist Land & Resources, Jinan 250013, Peoples R China
[6] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
基金
俄罗斯基础研究基金会; 中国国家自然科学基金;
关键词
Volcanic rocks; Sr-Nd-Pb isotopes; Magmatic source; Geodynamic evolution; Tianshan; PALEOZOIC TECTONIC EVOLUTION; TIEN-SHAN; TRACE-ELEMENT; CENTRAL-ASIA; GEOLOGICAL CHARACTERISTICS; CHEMICAL CLASSIFICATION; SOUTHWESTERN TIANSHAN; CONTINENTAL GROWTH; OCEANIC BASALTS; GRANITOID ROCKS;
D O I
10.1016/j.lithos.2015.04.019
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Awulale metallogenic belt (AMB) of the western Tianshan (NW China) includes Late Carboniferous (ca. 320 Ma) ore-bearing volcanic rocks of the Dahalajunshan Formation. The petrogenesis and tectonic setting of these volcanic rocks are important for the understanding of the tectonic evolution and metallogeny of the western Tianshan. This paper presents new major and trace elements and Sr-Nd-Pb isotope data from the Dahalajunshan volcanic rocks, which are mainly calc-alkaline basaltic trachy-andesite and trachy-andesite with subordinate basalt, trachy-basalt and rhyolite. The variations of major and trace elements in the mafic and intermediate volcanic rocks indicate the fractionation of pyroxene and magnetite or hornblende, magnetite, apatite and plagioclase, respectively, during their petrogenesis. The Dahalajunshan volcanic rocks have similar primitive mantle-normalized diagrams and chondrite-normalized rare-earth element (REE) patterns suggesting their similar mantle source(s). They are characterized by enrichment in large ion lithophile elements (LILEs) and light REEs (LREEs), depletion in heavy REEs (La-N/Yb-N approximate to 2.80 to 9.59) and high field strength elements (HFSEs) and epsilon(Nd)(t) ranging from +1.2 to +6.0 at Sr-86/Sr-87((t)) = 0.7047-0.7063 and Pb-206/Pb-204(i) = 17.49-18.19. Both the geochemical and isotopic data indicate that the volcanic rocks were probably derived by low-degree melting of sub-arc lithospheric mantle modified by fluids in a continental arc setting. Our obtained results, in conjunction with previous published data, allow us to suggest that the southward subduction of Junggar oceanic crust continued until the Late Carboniferous and was followed by a tectonic shift from continental arc to post-collisional extension environment. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:62 / 77
页数:16
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