Major zircon megacryst suites of the Indo-Pacific lithospheric margin (ZIP) and their petrogenetic and regional implications

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• 作者：Lin Sutherland ; Ian Graham ; Gregory Yaxley ; Richard Armstrong…
• 刊名：Mineralogy and Petrology
• 出版年：2016
• 出版时间：April 2016
• 年：2016
• 卷：110
• 期：2-3
• 页码：399-420
• 全文大小：995 KB
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• 作者单位：Lin Sutherland (1) (2)
  Ian Graham (1) (3)
  Gregory Yaxley (4)
  Richard Armstrong (4)
  Gaston Giuliani (5)
  Paul Hoskin (8)
  Victor Nechaev (6) (7)
  Jon Woodhead (9)
  
  1. Geoscience, Australian Museum, 6 College Street, Sydney, NSW, 2010, Australia
  2. School of Science and Health, Western Sydney University, Locked Bag 1797, Penrith South DC, NSW, 1797, Australia
  3. School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, 2052, Australia
  4. Research School of Earth Sciences, Australian National University, Canberra, ACT, 0200, Australia
  5. Université de Lorraine, CRPG UMR 7358 CNRS-UL, BP20, 54501, Vandoeuvre-lès-Nancy, France
  8. Department of Geology, University of Namibia, Private Bag 13301, Windhoek, Namibia
  6. Far East Geological Institute, 159, PR. 100-LET, Vladivostok, 690022, Russia
  7. Engineering School, Far Eastern Federal University, 8 Sukanova Str, Vladivostok, 690950, Russia
  9. School of Earth Sciences, University of Melbourne, Parkville, VIC, 3010, Australia
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Mineralogy
  Geochemistry
  
• 出版者：Springer Wien
• ISSN：1438-1168

文摘

Zircon megacrysts (± gem corundum) appear in basalt fields of Indo-Pacific origin over a 12,000 km zone (ZIP) along West Pacific continental margins. Age-dating, trace element, oxygen and hafnium isotope studies on representative zircons (East Australia–Asia) indicate diverse magmatic sources. The U–Pb (249 to 1 Ma) and zircon fission track (ZFT) ages (65 to 1 Ma) suggest thermal annealing during later basalt transport, with < 1 to 203 Ma gaps between the U–Pb and ZFT ages. Magmatic growth zonation and Zr/Hf ratios (0.01–0.02) suggest alkaline magmatic sources, while Ti—in—zircon thermometry suggests that most zircons crystallized within ranges between 550 and 830 °C. Chondrite-normalised multi-element plots show variable enrichment patterns, mostly without marked Eu depletion, indicating little plagioclase fractionation in source melts. Key elements and ratios matched against zircons from magmatic rocks suggest a range of ultramafic to felsic source melts. Zircon O-isotope ratios (δ18O in the range 4 to 11‰) and initial Hf isotope ratios (εHf in the range +2 to +14) encompass ranges for both mantle and crustal melts. Calculated Depleted Mantle (TDM 0.03–0.56 Ga) and Crustal Residence (0.20–1.02 Ga) model ages suggest several mantle events, continental break-ups (Rodinia and Gondwana) and convergent margin collisions left imprints in the zircon source melts. East Australian ZIP sites reflect prolonged intraplate magmatism (~85 Ma), often during times of fast-migrating lithosphere. In contrast, East Asian-Russian ZIP sites reflect later basaltic magmatism (<40 Ma), often linked to episodes of back-arc rifting and spreading, slow-migrating lithosphere and slab subduction.