neutralize
发表于 2025-3-25 07:05:38
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欢乐中国
发表于 2025-3-25 09:31:01
2193-8571 t and Mantle as well as chondritic meteoritesFluid-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 th
清晰
发表于 2025-3-25 12:14:39
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GRAIN
发表于 2025-3-25 17:53:50
Metasomatism and the Chemical Transformation of Rock: Rock-Mineral-Fluid Interaction in Terrestrialte. This process is mainly due to an adjustment of the rock to physical conditions that differ from those under which the rock originally formed and that also differ from the physical conditions normally occurring at the surface of the Earth and in the zone of diagenesis. The process may coexist wit
Misnomer
发表于 2025-3-25 21:32:40
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ALIAS
发表于 2025-3-26 03:56:51
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异端邪说下
发表于 2025-3-26 07:19:19
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CROW
发表于 2025-3-26 08:58:17
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inventory
发表于 2025-3-26 14:47:50
Geochronology of Metasomatic Events,e (as demonstrated for zircon, monazite, titanite, amphibole, K-feldspar, biotite, and muscovite). Metasomatic assemblages commonly contain such mixtures between relicts and newly formed phases, whose geochronology is slightly more complex than that of simple, ideal systems, but can be managed by te
含糊
发表于 2025-3-26 18:25:43
Metasomatism Within the Ocean Crust,. In heterogeneous crust (mixed mafic-ultramafic lithologies), however, diffusional mass transfers between basaltic lithologies and peridotite are very common. These processes include rodingitization of gabbroic dikes in the lithospheric mantle and steatitization of serpentinites in contact to gabbr