Startseite Naturwissenschaften Tracking the evolution of Late Mesozoic arc-related magmatic systems in Hong Kong using in-situ U-Pb dating and trace element analyses in zircon
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Tracking the evolution of Late Mesozoic arc-related magmatic systems in Hong Kong using in-situ U-Pb dating and trace element analyses in zircon

  • Denise L.K. Tang , Colin J.N. Wilson EMAIL logo , Roderick J. Sewell , Diane Seward , Lung S. Chan , Trevor R. Ireland und Joseph L. Wooden
Veröffentlicht/Copyright: 30. Oktober 2017
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American Mineralogist
Aus der Zeitschrift American Mineralogist Band 102 Heft 11

Abstract

The links between large-scale silicic volcanism and plutonism offer insights into the dynamics of crustal magmatic systems and growth of continental crust. In Hong Kong, voluminous silicic ignimbrites and linked plutons record a ~26 Myr period of magmatism from ~164 to 138 Ma. We present data from these linked volcanic-plutonic assemblages at the Lantau and High Island caldera complexes, with an emphasis on the ~143–138 Ma activity from the latter. To track the evolution of these magmatic systems, U-Pb dating and trace element analyses using secondary-ion mass spectrometry (SIMS) were carried out on zircons from 21 samples from both volcanic and plutonic samples. The SIMS age data sets divide into two groups across volcanic and plutonic origins: (1) seven samples with unimodal age spectra [five of which have the same mean value as the published Isotope Dilution Thermal Ionization Mass Spectrometry (ID-TIMS) age from the same sample]; and (2) 14 samples yielding multiple age components. Age patterns from both groups suggest that the previously separated ~143 Ma Repulse Bay (RBVG) and ~141–140 Ma Kau Sai Chau volcanic groups (KSCVG) instead represent activities over a single ~5 Myr period. Direct linkages previously proposed between some volcanic and plutonic units for this period (e.g., High Island Tuff, Kowloon Granite) are no longer supported, and magmatism represented by exposed plutons continued until 137.8 ± 0.8 Ma (Mount Butler Granite). Under CL imagery, a wide range of zircon textures identified in both volcanic and plutonic samples is indicative of complex processes, some of which are identified through trace element data coupled with textural characteristics. Overall, intra-grain (cores vs. rims; sector-zonation) and intra-sample variations in trace element abundances and ratios are larger than those between samples. Zircon chemistries in both volcanic and plutonic samples fall into two groups during the ~5 Myr history of the High Island caldera magmatic system. One group (RBVG and “cold” granites) includes inherited grains back to 164 Ma and wider ranges in Hf, Y, total trivalent elements, Th and U concentrations and Th/U, Yb/Gd, and U/Yb ratios than the other (KSCVG and “hot” granites). Two possible evolutionary models of the High Island caldera magmatic system are: (1) the system randomly tapped a single crustal domain that fluctuated in temperature as a result of varying interactions of hotter melts, or (2) the volcanic and plutonic records reflect the interplay of two crustal domains with contrasting “low-” and “high-temperature” characteristics. In Hong Kong, some plutonic bodies were comagmatic with large-scale volcanism, while others were emplaced at shallow crustal levels independently of volcanism, matching the current two end-member views of the volcanic-plutonic relationship.

Keywords: Volcanism; plutonism; granite; rhyolite; Hong Kong; Mesozoic; caldera; zircon

Acknowledgments

D.L.K.T acknowledges support from a Victoria University Doctoral Scholarship. C.J.N.W. acknowledges support from the Royal Society of New Zealand (Cook Fellowship, Marsden Fund grant VUW0813) and Victoria University (University Research Fund). L.S.C. acknowledges support from the research funding of the Department of Earth Sciences, Hong Kong University. We thank Matt Coble, Peter Holden, and Brad Ito for their support in the ion probe laboratory work. D.L.K.T. and R.J.S. publish with the permission from Head of Geotechnical Engineering Office and Director of Civil Engineering and Development Department. We thank Rich Gaschnig and Calvin Miller for their constructive comments, and Fang-Zhen Teng for editorial handling.

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Received: 2017-1-7
Accepted: 2017-6-23
Published Online: 2017-10-30
Published in Print: 2017-11-27

© 2017 Walter de Gruyter GmbH, Berlin/Boston

Artikel in diesem Heft

  1. Highlights and Breakthroughs
  2. Rutile: A novel recorder of high-fo2 fluids in subduction zones
  3. Highlights and Breakthroughs
  4. Granites and rhyolites: Messages from Hong Kong, courtesy of zircon
  5. Review
  6. Do Fe-Ti-oxide magmas exist? Probably not!
  7. Special Collection: Biomaterials—Mineralogy Meets Medicine
  8. Calcium (Ti,Zr) hexaorthophosphate bioceramics for electrically stimulated biomedical implant devices: A position paper
  9. Special Collection: Water in Nominally Hydrous and Anhydrous Minerals
  10. Raman spectroscopy of water-rich stishovite and dense high-pressure silica up to 55 GPa
  12. Tracking the evolution of Late Mesozoic arc-related magmatic systems in Hong Kong using in-situ U-Pb dating and trace element analyses in zircon
  14. Defect contributions to the heat capacities and stabilities of some chain, ring, and sheet silicates, with implications for mantle minerals
  16. Phase transition in SiC from zinc-blende to rock-salt structure and implications for carbon-rich extrasolar planets
  18. Non-destructive, multi-method, internal analysis of multiple inclusions in a single diamond: First occurrence of mackinawite (Fe,Ni)1+xS
  20. The fate of ammonium in phengite at high temperature
  22. Parameterized lattice strain models for REE partitioning between amphibole and silicate melt
  24. Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins (Dabie UHP terrane): A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs
  26. Crystallization experiments in rhyolitic systems: The effect of temperature cycling and starting material on crystal size distribution
  28. Dolomite dissociation indicates ultra-deep (>150 km) subduction of a garnet-bearing dunite block (the Sulu UHP terrane)
  30. Microscopic strain in a grossular-pyrope solution anti-correlates with excess volume through local Mg-Ca cation arrangement, more strongly at high Ca/Mg ratio
  32. Ferruginous seawater facilitates the transformation of glauconite to chamosite: An example from the Mesoproterozoic Xiamaling Formation of North China
  34. Charleshatchettite, CaNb4O10(OH)2·8H2O, a new mineral from Mont Saint-Hilaire, Québec, Canada: Description, crystal-structure determination, and origin
  36. New Mineral Names
  38. Erratum
  39. Book Review
  40. Non-Traditional Stable Isotopes
https://doi.org/10.2138/am-2017-6071
Schlagwörter für diesen Artikel
Volcanism; plutonism; granite; rhyolite; Hong Kong; Mesozoic; caldera; zircon

Artikel in diesem Heft

  1. Highlights and Breakthroughs
  2. Rutile: A novel recorder of high-fo2 fluids in subduction zones
  3. Highlights and Breakthroughs
  4. Granites and rhyolites: Messages from Hong Kong, courtesy of zircon
  5. Review
  6. Do Fe-Ti-oxide magmas exist? Probably not!
  7. Special Collection: Biomaterials—Mineralogy Meets Medicine
  8. Calcium (Ti,Zr) hexaorthophosphate bioceramics for electrically stimulated biomedical implant devices: A position paper
  9. Special Collection: Water in Nominally Hydrous and Anhydrous Minerals
  10. Raman spectroscopy of water-rich stishovite and dense high-pressure silica up to 55 GPa
  12. Tracking the evolution of Late Mesozoic arc-related magmatic systems in Hong Kong using in-situ U-Pb dating and trace element analyses in zircon
  14. Defect contributions to the heat capacities and stabilities of some chain, ring, and sheet silicates, with implications for mantle minerals
  16. Phase transition in SiC from zinc-blende to rock-salt structure and implications for carbon-rich extrasolar planets
  18. Non-destructive, multi-method, internal analysis of multiple inclusions in a single diamond: First occurrence of mackinawite (Fe,Ni)1+xS
  20. The fate of ammonium in phengite at high temperature
  22. Parameterized lattice strain models for REE partitioning between amphibole and silicate melt
  24. Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins (Dabie UHP terrane): A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs
  26. Crystallization experiments in rhyolitic systems: The effect of temperature cycling and starting material on crystal size distribution
  28. Dolomite dissociation indicates ultra-deep (>150 km) subduction of a garnet-bearing dunite block (the Sulu UHP terrane)
  30. Microscopic strain in a grossular-pyrope solution anti-correlates with excess volume through local Mg-Ca cation arrangement, more strongly at high Ca/Mg ratio
  32. Ferruginous seawater facilitates the transformation of glauconite to chamosite: An example from the Mesoproterozoic Xiamaling Formation of North China
  34. Charleshatchettite, CaNb4O10(OH)2·8H2O, a new mineral from Mont Saint-Hilaire, Québec, Canada: Description, crystal-structure determination, and origin
  36. New Mineral Names
  38. Erratum
  39. Book Review
  40. Non-Traditional Stable Isotopes
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