What caused the Early Silurian change from mafic to silicic (S‐type) magmatism in the eastern Lachlan Fold Belt?-Reference-Cited by-同舟云学术

What caused the Early Silurian change from mafic to silicic (S‐type) magmatism in the eastern Lachlan Fold Belt?

Published:2001-02-01 Issue:1 Volume:48 Page:25-41
ISSN:0812-0099
Container-title:Australian Journal of Earth Sciences
language:en
Short-container-title:Australian Journal of Earth Sciences

Author:

Collins W. J.¹,Hobbs B. E.²

Affiliation:

1. a Department of Geology , University of Newcastle , Newcastle, NSW, 2308, Australia

2. b Australian Geodynamics CRC , CSIRO Exploration and Mining , Private Bag, PO Wembley, WA, 6014, Australia

Publisher

Informa UK Limited

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Link

https://www.tandfonline.com/doi/pdf/10.1046/j.1440-0952.2001.00837.x

Reference97 articles.

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2. Anderson, J. A. C. and Price, R. C. and Fleming, P. D. (1996) Structural analysis of metasedimentary enclaves: implications for tectonic evolution and granite petrogenesis in the southern Lachlan Fold Belt, Australia Geology, 26, pp. 119 - 122.

3. Anderson, J. A. C. and Williams, I. S. and Price, R. C. and Fleming, P. D. (1998) U–Pb zircon ages from the Koetong adamellite: implications for granite genesis and the local basement in NE Victoria Geological Society of Australia Abstracts, 42, pp. 1 - 2.

4. Atherton, M. P. (1990) The Coastal Batholith of Peru: the product of rapid recycling of ‘new’ crust formed within rifted continental margin Geological Journal, 25, pp. 337 - 349.

5. Carr, G. R. and Dean, J. A. and Suppel, D. W. and Heithersay, P. S. (1995) Precise lead isotopic fingerprinting of hydrothermal activity associated with Ordovician to Carboniferous metallogenic events in the Lachlan Fold Belt of New South Wales Economic Geology, 90, pp. 1467 - 1505.

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