Titlebook: Ophiolite Genesis and Evolution of the Oceanic Lithosphere; Proceedings of the O Tj. Peters,A. Nicolas,R. G. Coleman Conference proceedings

Hemochromatosis

書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere影響因子(影響力)




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere影響因子(影響力)學(xué)科排名




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere網(wǎng)絡(luò)公開度




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere被引頻次




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere被引頻次學(xué)科排名




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere年度引用




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere年度引用學(xué)科排名




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere讀者反饋




書目名稱Ophiolite Genesis and Evolution of the Oceanic Lithosphere讀者反饋學(xué)科排名

令人心醉

https://doi.org/10.1007/978-94-011-3358-6Coast; Ocean; dike; fault; igneous rock; marine; obduction; subduction; tectonics

無效

978-94-010-5484-3Ministry of Petroleum and Minerals, Sultanate of Oman 1991

cruise

Ophiolite Genesis and Evolution of the Oceanic Lithosphere978-94-011-3358-6Series ISSN 0924-1957

產(chǎn)生

粗糙

Introductionphiolites has provided a wealth of insight into lithospheric processes and has proved to be an indispensible prerequisite to interpreting geophysical and other investigations of the crust underlying recent oceans. The Oman Ophiolite offers the most complete and structurally undisturbed sections of t

十字架

行業(yè)

Platinum-Group Elements and Gold in Ophiolitic Complexes: Distribution and Fractionation from Mantlep Elements (PGE) are nearly unfractionated in the less depleted mantle rocks (lherzolites). Residual dunites are clearly empoverished in Pt, Pd, and Au which were collected by silicate melts during partial melting. The chromite grains of the podiform chromitites, which crystallized early in magmatic

修剪過的樹籬

Chromite-Rich and Chromite-Poor Ophiolites: The Oman Casectonically rotated to become parallel to the peridotite foliation. This occurred soon after their formation within the transition zone below the ridge of origin. Subconcordant and discordant pods are also present. The latter have preserved delicate magmatic structures showing that they have only bee

敏捷