Výsledky vyhledávání - "B. W. Chappell"

Towards a unified model for granite genesis

Autor: B. W. Chappell

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 95:1-10

Most granites result from partial melting within the crust. Granite melts produced at the lowest temperatures of partial melting mainly comprise close to equal amounts of the haplogranite components Qz, Ab and Or, with H2O. Many felsic granites were

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c446bb3ffb29084e3f73523f8e7b64d7
https://doi.org/10.1017/s0263593300000870

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Granite suites and supersuites of eastern Australia

Autor: Lesley Wyborn, B. W. Chappell, S. D. Beams, D. Wyborn, A. J. R. White, Paul F. Carr, David C. Champion, Charlotte M. Allen

Publikováno v: Australian Journal of Earth Sciences. 48:515-530

Separate granite plutons in southeastern Australia can commonly be grouped into suites on the basis of shared similarities in field, petrographic and compositional data. Granites in different plutons of the same suite share common properties or exhib

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::df83b17ee909f3fcaa8b405c1a6157da
https://doi.org/10.1046/j.1440-0952.2001.00874.x

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Three S-Type Volcanic Suites From the Lachlan Fold Belt, Southeast Australia

Autor: D. Wyborn, B. W. Chappell, R. M. Johnston

Publikováno v: 1989, Granites and Rhyolites ISBN: 9781118782057

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::212227d2419b27e9d7ab52f617e99b38
https://doi.org/10.1002/9781118782057.ch12

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Discussion and Reply: Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: Implications for crustal architecture and tectonic models

Autor: B. W. Chappell, A. J. R. White, I. S. Williams, D. Wyborn, J. M. Hergt, J. D. Woodhead, W. J. Collins

Publikováno v: Australian Journal of Earth Sciences. 46:827-836

(1999). Discussion and Reply: Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: Implications for crustal architecture and tectonic models. Australian Journal of Earth Sciences: Vol. 46, No. 5, pp. 827-836.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::94a77cb58953cfb0a8a58a18a8777cff
https://doi.org/10.1046/j.1440-0952.1999.00742.x

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Compositional variation within granite suites of the Lachlan Fold Belt: its causes and implications for the physical state of granite magma

Autor: B. W. Chappell

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 87:159-170

Granites within suites share compositional properties that reflect features of their source rocks. Variation within suites results dominantly from crystal fractionation, either of restite crystals entrained from the source, or by the fractional cryst

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::458518d5c336d0217071830cdfd2eeb1
https://doi.org/10.1017/s026359330000657x

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I- and S-type granites in the Lachlan Fold Belt

Autor: B. W. Chappell, A. J. R. White

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 83:1-26

Granites and related volcanic rocks of the Lachlan Fold Belt can be grouped into suites using chemical and petrographic data. The distinctive characteristics of suites reflect source-rock features. The first-order subdivision within the suites is bet

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c6a1814e1213bfebcd60c775571348b7
https://doi.org/10.1017/s0263593300007720

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The Cretaceous volcanic-plutonic province of the central Queensland (Australia) coast—a rift related ‘calc-alkaline’ province

Autor: A. Ewart, R. W. Schon, B. W. Chappell

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 83:327-345

Silicic and minor intermediate and mafic pyroclastics, lavas, and dykes occupy a NW-trending zone through the Whitsunday, Cumberland and Northumberland Island groups, and locally areas on the adjacent mainland, over a distance of more than 300 km alo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::0be932aec55b56f6523ccd5cd0ee1c37
https://doi.org/10.1017/s0263593300008002

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