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Granites of the southern Mongolia Carboniferous arc : new geochronological and geochemical constraints

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  • المؤلفون: Blight, James H.S.; Crowley, Quentin G.; Petterson, Michael G.; Cunningham, Dickson
  • نوع التسجيلة:
    Electronic Resource
  • الدخول الالكتروني :
    http://nora.nerc.ac.uk/id/eprint/9545/1/The_crust_in_southern_Mongolia_is_part_of_the_Central_Asian_Orogenic_Belt.pdf
    http://nora.nerc.ac.uk/id/eprint/9545/
    http://www.sciencedirect.com/science/journal/00244937
    http://nora.nerc.ac.uk/id/eprint/9545
    http://www.sciencedirect.com/science/journal/00244937
    10.1016/j.lithos.2010.01.001
  • معلومة اضافية
    • Publisher Information:
      Elsevier 2010
    • نبذة مختصرة :
      The crust in southern Mongolia is part of the Central Asian Orogenic Belt, a vast accretionary orogen that records the opening and closure of the Palaeo-asian Ocean in the late Proterozoic to Palaeozoic. The crustal evolution of the region is revealed in basement inliers that also contain intrusion-related porphyry ore bodies that are important mineral exploration targets. The Saykhandulaan inlier in Southeast Mongolia is a Devonian–Carboniferous segment of island-arc crust, which is dominantly composed of extrusive and sedimentary lithologies, but which also contains the Oyut Ulaan I-type quartz-monzonite intrusion. A U–Pb zircon age for the Oyut Ulaan monzonite indicates emplacement at 330.0 ± 0.5 Ma. To the east of the Saykhandulaan inlier, intrusive complexes dominate the neighbouring Mandakh inlier. New ages are presented for four of these plutons; the Bronze Fox granodiorite (333.6 ± 0.6 Ma); the Narin Hudag monzonite (333.2 ± 0.6 Ma); the Shuteen quartz monzonite (325.5 ± 1.0 Ma); and the North Mandakh granite (292.3 ± 0.5). The intrusive bodies of the Saykhandulaan and Mandakh inliers have two distinct geochronological and geochemical associations: 1) mid-Carboniferous I-type monzonites that constitute the most easterly intrusive expression of the Southern Mongolia Carboniferous Arc and, 2) Early Permian A-type and peralkaline granites that represent a post-orogenic phase of voluminous granite emplacement. Both groups are significantly younger than the nearby Oyu Tolgoi and Tsagaan Suvarga Cu-porphyry ore bodies, which have previously been dated as early- and late-Devonian respectively. The new data presented here provide constraints on the timing of the transition from island-arc magmatism to post-collisional extension-related magmatism in the region and possible controls on fertile and infertile granitoid intrusions with respect to Cu–Au mineralisation.
    • الموضوع:
    • Availability:
      Open access content. Open access content
    • Note:
      text
      English
    • Other Numbers:
      UKNRA oai:nora.nerc.ac.uk:9545
      Blight, James H.S.; Crowley, Quentin G.; Petterson, Michael G.; Cunningham, Dickson. 2010 Granites of the southern Mongolia Carboniferous arc : new geochronological and geochemical constraints. Lithos, 116 (1-2). 35-52. https://doi.org/10.1016/j.lithos.2010.01.001
      703250022
    • Contributing Source:
      NERC OPEN RES ARCH
      From OAIster®, provided by the OCLC Cooperative.
    • الرقم المعرف:
      edsoai.ocn703250022
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