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Titlebook: Orogenic Andesites and Plate Tectonics; James B. Gill Book 1981 Springer-Verlag Berlin · Heidelberg 1981 Andesit.environment.evolution.for

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發(fā)表于 2025-3-21 20:05:32 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Orogenic Andesites and Plate Tectonics
編輯James B. Gill
視頻videohttp://file.papertrans.cn/705/704668/704668.mp4
叢書名稱Minerals, Rocks and Mountains
圖書封面Titlebook: Orogenic Andesites and Plate Tectonics;  James B. Gill Book 1981 Springer-Verlag Berlin · Heidelberg 1981 Andesit.environment.evolution.for
描述Students of a phenomenon as common but complex as andesite genesis often are overwhelmed by, or overlook, the volume and diversity of relevant information. Thus there is need for periodic overview even in the absence of a dramatic breakthrough which "solves the andesite problem" and even though new ideas and data keep the issues in a state of flux. Thus I have summarized the subject through mid·1980 from my perspective to help clarify the long-standing problem and to identify profitable areas for future research. Overviews are more easily justified than achieved and there are fundamental differences of opinion concerning how to go about them. It is professionally dangerous and therefore uncom- mon for single authors, especially those under 35 such as I, to summarize a broad, active field of science in book-length thor- oughness. Review articles in journals, multi-authored books, or symposia proceedings appear instead. The single-authored approach is intimidating in scale and can result in loss of thoroughness or authority on individual topics. The alternatives lack scope or integration or both.
出版日期Book 1981
關鍵詞Andesit; environment; evolution; formation; integration; lithosphere; mineral; mineralogy; plate tectonics; r
版次1
doihttps://doi.org/10.1007/978-3-642-68012-0
isbn_softcover978-3-642-68014-4
isbn_ebook978-3-642-68012-0Series ISSN 0343-2181
issn_series 0343-2181
copyrightSpringer-Verlag Berlin · Heidelberg 1981
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The Plate Tectonic Connection,anism is concentrated at plate boundaries or in linear belts or local magma floods, usually of basalt, in intra-plate locations. Andesites occur in all four environments. However, orogenic andesites are associated primarily with convergent plate boundaries, and this association is the significance o
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Bulk Chemical Composition of Orogenic Andesites,n be used to test genetic hypotheses and to compare volcanic rocks from different areas or ages (between-suite comparisons). Second, variation in the concentration of elements or ratio of isotopes within suites must also be consistent with the differentiation mechanisms proposed (within-suite variat
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Mineralogy and Mineral Stabilities,mes providing Earth’s finest examples of anorthite and of coexisting pigeonite and hypersthene. However, most studies of andesite report only the identity or, at most, the proportion of phenocrysts present. Indeed, the isotopic composition of Sr is known for more andesites than is the composition of
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