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Titlebook: Origin of Granite Batholiths Geochemical Evidence; Based on a meeting o M. P. Atherton,J. Tarney Book 1979 M.P. Atherton and J. Tarney 1979

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发表于 2025-3-21 16:11:39 | 显示全部楼层 |阅读模式
书目名称Origin of Granite Batholiths Geochemical Evidence
副标题Based on a meeting o
编辑M. P. Atherton,J. Tarney
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图书封面Titlebook: Origin of Granite Batholiths Geochemical Evidence; Based on a meeting o M. P. Atherton,J. Tarney Book 1979 M.P. Atherton and J. Tarney 1979
描述This book is for undergraduates, postgraduates and research workers who wish to gain an insight into present ideas and speculations on the origin of granite batholiths. It is a summary of the proceedings of a one-day meeting of the Geochemistry Group of the Mineralogical Society held at the University of liverpool on the 2nd May 1979, entitled The Origin of Granite Batholiths: Geochemical Evidence. It was felt that relevant new geochemical and isotopic data with associated field and petrological observations would be helpful in clarifying the main issues connected with the origin of granitic rocks. The speakers who participated contri­ buted a wealth of data and ideas to the problem, based on many years‘ experience of granitic rocks in various parts of the world. The popularity of the meeting indicated that a summary of the talks might be welcomed by a wider audience; hence this book. For reasons of length and cost, authors have been limited to presenting only the essential results necessary to develop their arguments and ideas. The comprehensive reference list will, however, assist those who wish to pursue specific aspects in greater detail. Inevitably, the cost and speed of publi
出版日期Book 1979
关键词Batholith; chemistry; evolution; geochemistry; geology; granite; isotope; mineral; research; science
版次1
doihttps://doi.org/10.1007/978-1-4684-0570-5
isbn_softcover978-1-4684-7990-4
isbn_ebook978-1-4684-0570-5
copyrightM.P. Atherton and J. Tarney 1979
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发表于 2025-3-21 23:31:15 | 显示全部楼层
Compositional Variation in the Galloway Plutons, particular interest for two reasons, namely, that they show marked diversity in overall composition from basic diorites to muscovite granites, and also that the plutons exhibit striking petrological zoning. Our objective in this study was to understand the causes of the petrological variation both
发表于 2025-3-22 04:19:21 | 显示全部楼层
Isotope and Trace Element Evidence for the Origin and Evolution of Caledonian Granites in the Scott Sr-isotope geology were laid down by Faure and Hurley (1963). In general, it has been shown that granites display a very wide range of initial Sr and Pb-isotope compositions, open to an equally wide range of interpretations. Thus, Faure and Powell (1972) summarized the Sr-isotope data by recognizin
发表于 2025-3-22 07:26:00 | 显示全部楼层
Granite Magmatism in the Tin Belt of South-East Asia,in production (about 230 000 tonnes) is currently valued at about 3 x 109 US dollars and about 60% of this production comes from SE Asia. More dramatically, it is estimated that this metallogenic province has yielded about three-quarters of the world’s total tin production during the present century
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The Geochemical Character of the Segmented Peruvian Coastal Batholith and Associated Volcanics, of Liverpool and the Institute of Geological Sciences (see Pitcher, 1978). These studies have been predominantly concerned with the detailed mapping of the batholith, its stratigraphic and structural setting, and with the petrographic variation.
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Petrogenetic Relationships of Volcanic and Intrusive Rocks of the Andes,South Peru and North Chile, and a southern zone in South Chile (Figure 1). Cenozoic intrusive rocks occur between these areas, and on the coastal margin of the active zones. It is therefore natural to suppose that the igneous processes that take place along the Andean plate margin have simultaneous
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1 4 3Nd/1 4 4Nd, 8 7Sr/8 6Sr and Trace Element Characteristics of Magmas along Destructive Plate Mapirically they may help to resolve whether particular magmatic associations are related to one another, but their real potential lies in the detection of different components which may contribute to magmas in this tectonic environment.
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An Emplacement Mechanism for Post-Tectonic Granites and Its Implications for Their Geochemical Featand/or contamination. It is the purpose of this contribution, however, to examine what effect the intrusion mechanism of post-tectonic plutons has in the production of such zoning. To this end, the Ardara pluton, which has become one of the classic examples of a zoned post-tectonic pluton (Akaad, 19
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