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Titlebook: Archaean Geochemistry; The Origin and Evolu A. Kr?ner,G. N. Hanson,A. M. Goodwin Conference proceedings 1984 Springer-Verlag Berlin Heidelb

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發(fā)表于 2025-3-21 18:17:47 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱(chēng)Archaean Geochemistry
期刊簡(jiǎn)稱(chēng)The Origin and Evolu
影響因子2023A. Kr?ner,G. N. Hanson,A. M. Goodwin
視頻videohttp://file.papertrans.cn/162/161164/161164.mp4
圖書(shū)封面Titlebook: Archaean Geochemistry; The Origin and Evolu A. Kr?ner,G. N. Hanson,A. M. Goodwin Conference proceedings 1984 Springer-Verlag Berlin Heidelb
影響因子Archaean Geochemistry 1972 - 1984 The realisation that the continental crust contains well-preserved relics which date as far back as 4/5 of the Earth‘s age has given a great impetus to the study of early Precambrian terrains. As late as the mid-sixties the Archaean still constituted the ‘terra-in- cognita‘ of earth science. High metamorphic grades, poor out- crop, and not least a widely assumed obliteration of early crustal records by convective recycling and thermal reworking had com- bined to discourage research in this field. Many excellent local studies existed, notably around gold mining centres, but remained unrelated to a broader regional and theoretical understanding. This situation has changed as the consequence of two inter-related factors: (1) advances in isotopic methods and their application to Precambrian rocks, and (2) the recognition that some of the oldest terrains have retained a wealth of primary igneous and sedi- mentary textures and even geochemical characteristics.
Pindex Conference proceedings 1984
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Geochemical Characteristics of Archaean Ultramafic and Mafic Volcanic Rocks: Implications for Mantlat least for the upper mantle, was completed before 3.8 Ga ago. Moreover, a significant degree of mantle-crust and/or intra-mantle differentiation in the pre-Archaean (>3.8 Ga) is indicated by Nd and Sr isotopic data..Chondritic ratios for refractory lithophile elements (e.g. Al, Ti, Zr, Y, REE) are
板凳
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Archaean Sedimentary Rocks and Their Relation to the Composition of the Archaean Continental Crust,thought to reflect the composition of the exposed upper continental crust. In contrast, Archaean sedimentary rocks display highly variable trace element abundances, but on average have lower levels of incompatible elements (Th, LREE), lower La/Yb ratios and lack the Eu depletion characteristic of po
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Origin of Archaean Charnockites from Southern India,a continuous series exists from mafic to tonalite-trondhjemite end members. With the exception of K.O, major element distributions reflect the original igneous parentage of the rocks. Rb, Cs, Th, U, and Pb are depleted in charnockites although the degree of depletion does not correlate well with inf
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Radiometric Ages (Rb-Sr, Sm-Nd, U-Pb) and REE Geochemistry of Archaean Granulite Gneisses from East and trace element geochemistry. A consistent age of about 2.5 Ga has been obtained by the Rb-Sr and Sm-Nd whole-rock isochron methods, in agreement with the zircon U-Pb data (Pidgeon 1980; Liu et al. 1984). Geochemical arguments from initial isotopic ratios (I. and I.) and elemental distribution pa
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