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只看該作者 · 發(fā)表于 2025-3-21 17:01:31

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution影響因子(影響力)

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution影響因子(影響力)學(xué)科排名

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution網(wǎng)絡(luò)公開度

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution網(wǎng)絡(luò)公開度學(xué)科排名

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution被引頻次

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution被引頻次學(xué)科排名

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution年度引用

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution年度引用學(xué)科排名

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution讀者反饋

書目名稱Granite Genesis: In-Situ Melting and Crustal Evolution讀者反饋學(xué)科排名

只看該作者 · 發(fā)表于 2025-3-21 23:31:58

只看該作者 · 發(fā)表于 2025-3-22 01:50:09

只看該作者 · 發(fā)表于 2025-3-22 07:12:36

Introduction,amorphic, the material source of metamorphic rocks need not be considered because its predecessor is also rock. Igneous rocks derived by crystallisation of liquids can be divided into mafic and felsic end members represented by gabbro/basalt and granite/rhyolite, respectively, with different sources.

只看該作者 · 發(fā)表于 2025-3-22 10:25:54

Differentiation of magma layer: geochemical considerations,This means that the current paradigm of the magma intrusion model to explain the origin of granite is uncertain, and if granites are not derived from exogenic sources then geochemical data relating to their origin needs to be re-evaluated.

只看該作者 · 發(fā)表于 2025-3-22 16:39:57

只看該作者 · 發(fā)表于 2025-3-22 18:53:14

只看該作者 · 發(fā)表于 2025-3-23 01:11:28

Irena Maliszewska,Katarzyna Popkointensity mineralisation involving Au, Ag, Cu, Pb, Zn, Pb, Sb, W, Sn, Mo, Bi, Li, Be, Ta, Nb and REE is related to the Mesozoic tectonism/granite formation (Hua 1999) (Fig. 6.1), and many of these occurrences are described below.

只看該作者 · 發(fā)表于 2025-3-23 02:02:57

只看該作者 · 發(fā)表于 2025-3-23 05:44:24

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