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Anders Scherstén

Anders Scherstén

Senior lecturer

Anders Scherstén

Origin and geodynamic setting of Late Cenozoic granitoids in Sulawesi, Indonesia

Author

  • Adi Maulana
  • Akira Imai
  • Theo Van Leeuwen
  • Koichiro Watanabe
  • Kotaro Yonezu
  • Takanori Nakano
  • Adrian Boyce
  • Laurence Page
  • Anders Schersten

Summary, in English

Late Cenozoic granitoids are widespread in a 1600km long belt forming the Western and Northern Sulawesi tectono-magmatic provinces. They can be divided into three rock series: shoshonitic (HK), high-K felsic calc-alkaline (CAK), and normal calc-alkaline to tholeiitic (CA-TH). Representative samples collected from eleven plutons, which were subjected to petrography, major element, trace element, Sr, Nd, Pb isotope and whole-rock δ18O analyses, are all I-type and metaluminous to weakly peraluminous. The occurrence of the two K-rich series is restricted to Western Sulawesi, where they formed in an extensional, post-subduction tectonic setting with astenospheric upwelling providing thermal perturbation and adiabatic decompression. Two parental magma sources are proposed: enriched mantle or lower crustal equivalent for HK magmas, and Triassic igneous rocks in a Gondwana-derived fragment thrust beneath the cental and northern parts of Western Sulawesi for CAK magmas. The latter interpretation is based on striking similarities in radiogenic isotope and trace element signatures. CA-TH granitoids are found mostly in Northern Sulawesi. Partial melting of lower-middle crust amphibolites in an active subduction environment is the proposed origin of these rocks. Fractional crystallization and crustal contamination have played a significant role in magma petrogenesis, particularly in the case of the HK and CAK series. Contamination by organic carbon-bearing sedimentary rocks of the HK and CAK granitoids in the central part of Western Sulawesi is suggested by their ilmenite-series (reduced) character. The CAK granitoids further to the north and CA-TH granitoids in Northern Sulawesi are typical magnetite-series (oxidized). This may explain differences in mineralization styles in the two regions.

Department/s

  • Lithosphere and Biosphere Science

Publishing year

2016-07-01

Language

English

Pages

102-125

Publication/Series

Journal of Asian Earth Sciences

Volume

124

Document type

Journal article

Publisher

Elsevier

Topic

  • Geology

Keywords

  • Geodynamic setting
  • Granitoid
  • Indonesia
  • Petrogenesis
  • Source protoliths
  • Sulawesi

Status

Published

ISBN/ISSN/Other

  • ISSN: 1367-9120