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Titlebook: Metal Deposits in Relation to Plate Tectonics; Frederick J. Sawkins Book 19841st edition Springer-Verlag Berlin Heidelberg 1984 Deposits.E

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書(shū)目名稱(chēng)Metal Deposits in Relation to Plate Tectonics
編輯Frederick J. Sawkins
視頻videohttp://file.papertrans.cn/632/631412/631412.mp4
叢書(shū)名稱(chēng)Minerals, Rocks and Mountains
圖書(shū)封面Titlebook: Metal Deposits in Relation to Plate Tectonics;  Frederick J. Sawkins Book 19841st edition Springer-Verlag Berlin Heidelberg 1984 Deposits.E
描述I attempt this volume with no small degree of trepidation, for despite the near universal acceptance of plate tectonic theory, and the undeniable sweep and power of the concepts in- volved, points of controversy and uncertainty still abound. This is especially true with regard to the limited extent to which many ancient geologic terrains, however well studied, lend themselves to plate tectonic interpretation. There is also considerable controversy regarding the genesis of many metal deposits, and this impacts upon the degree to which such deposits can be meaningfully related to the tectonic settings in which they occur. It is relatively simple matter to point out that certain types of ore deposits exhibit impressive time-space associations with certain kinds of more recent plate boundary environ- ments. It is also all too easy to possible plate tectonic-ore deposit relationships in ancient geologic terrains. What is more challenging is the recognition of the boundaries beyond which speculation is idle, but within which useful new insights regarding the relationship of certain ores to their lithologic and tectonic environments may emerge.
出版日期Book 19841st edition
關(guān)鍵詞Deposits; Erzlagerst?tte; Plattentektonik; Relation; plate tectonics; mineral resources
版次1
doihttps://doi.org/10.1007/978-3-642-96785-6
isbn_ebook978-3-642-96785-6Series ISSN 0343-2181
issn_series 0343-2181
copyrightSpringer-Verlag Berlin Heidelberg 1984
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Metal Deposits Associated with the Early Stages of Continental Rifting deposits, but in this chapter I will consider metal deposits that tend to form in continental rift settings. As stated so aptly by Mohr (1982), “sufficient unto rift valleys are the existing models thereof.” Mohr stresses the complexity and variability of rift systems and the need to re-examine som
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