| 书目名称 | Metasomatism and the Chemical Transformation of Rock |
| 副标题 | The Role of Fluids i |
| 编辑 | Daniel E. Harlov,Håkon Austrheim |
| 视频video | |
| 概述 | A complete state-of-the-art review of metasomatism.Written by leading experts in the field.Reviews metasomatic processes in the Earth‘s Crust and Mantle as well as chondritic meteorites |
| 丛书名称 | Lecture Notes in Earth System Sciences |
| 图书封面 |  |
| 描述 | Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observatio |
| 出版日期 | Book 2013 |
| 关键词 | Fluid; Geochemistry; Mass-transfer; Metamorphism; Metasomatism |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-642-28394-9 |
| isbn_softcover | 978-3-662-52064-2 |
| isbn_ebook | 978-3-642-28394-9Series ISSN 2193-8571 Series E-ISSN 2193-858X |
| issn_series | 2193-8571 |
| copyright | Springer-Verlag Berlin Heidelberg 2013 |
发表于 2025-3-21 16:27:48
