4.6 Article

Late Triassic high-Mg andesite/dacite suites from northern Hohxil, North Tibet: Geochronology, geochemical characteristics, petrogenetic processes and tectonic implications

期刊

LITHOS
卷 126, 期 1-2, 页码 54-67

出版社

ELSEVIER
DOI: 10.1016/j.lithos.2011.06.002

关键词

High-Mg andesite; Adakite; Triassic; Subduction; Songpang-Gangzi; Tibet

资金

  1. Chinese Academy of Sciences [KZCX2-YW-Q09-05-01]
  2. National Natural Science Foundation of China [41025006, 41073029]
  3. Major State Basic Research Program of People's Republic of China [2007CB411308, 2009CB421004]
  4. Institute for Geoscience Research (TIGeR) at Curtin University of Technology

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This study reports age, petrologic and geochemical data for andesites and dacites from the Late Triassic sedimentary strata of northern Hohxil, in the Hohxil-Songpan-Ganzi Block (northern Tibet), which constitutes the most voluminous Triassic strata on Earth. LA-ICP-MS zircon U-Pb analysis of dacite (210.4 +/- 1.9 Ma) and whole rock 40Ar-39Ar analyses for both the andesites and dacites (211 +/- 2 Ma and 210.9 +/- 1.6 Ma) show that the rocks were almost contemporaneous. Both rock types are sodium-rich and calc-alkaline. The andesites, characterized by high MgO (up to 10 wt.%) or Mg-# (similar to 70), TiO2, Al2O3, Cr, Ni, La/Yb and Th/La, but low Nb/Ta ratios, are geochemically similar to sanukitoids in southeastern Japan. The dacites are strongly peraluminous, and have high Al2O3 and La/Yb, low Y and Yb, coupled with negligible to positive Eu and Sr anomalies, comparable to slab-derived adakites in the circum Pacific arc system. Both rocks exhibit strongly fractionated platinum group element patterns, with Pt/Pt* (Pt anomaly), (Pt/Ir)(N) and Re/Os ratios higher than those of the primitive mantle. They have uniformly low epsilon Nd(t) values (-7.57--9.59) and high (Sr-86/Sr-87)(i) ratios (0.7086-0.7106) that imply a continental rather than oceanic type magma source. We suggest that the northern Hohxil dacites were produced by partial melting of subducted sediments on the northward-subducting Songpan-Ganzi oceanic slab, and the high-Mg andesites were formed by subsequent interaction between the sediment-derived melts and mantle wedge peridotites. Taking into account the Triassic magmatic record from nearby regions, we suggest that the Late Triassic high-Mg andesite/dacite suites of northern Hohxil were generated in a forearc setting, and propose that double-sided subduction eventually closed the Songpan-Ganzi ocean during the Late Triassic. (C) 2011 Elsevier B.V. All rights reserved.

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