Petrogenesis and tectonic significance of the Baipu granite porphyry in the Huangtian uranium deposit, northeastern Guangdong, South China. [PDF]
Ruan K, Wu J, Long Z, Min Z.
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A computed tomography observation of the Unzen lava reveals the frequent existence of vesicles and crystals in proximity. [PDF]
Saito K, Hoshino M, Goto A, Namiki A.
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Initial Conditions of Planet Formation: Time Constraints from Small Bodies and the Lifetime of Reservoirs in the Solar Protoplanetary Disk. [PDF]
Schönbächler M +3 more
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Coupled sulfur-silicon isotopes reveal supracrustal origin of Archean continents. [PDF]
Shang K +8 more
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A shallow mantle source for the Chang'e 5 lavas reveals how top-down heating prolonged lunar magmatism. [PDF]
Elardo SM +4 more
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Widespread ilmenite contributions to the surface water cycle in lunar Procellarum KREEP Terrane. [PDF]
Xu Y +16 more
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Constraints of middle-late Permian granites in Eastern Inner Mongolia on the final subduction of the Paleo Asian Ocean. [PDF]
Zhao C, Yu Y, Liu Y, Cai H, He J, Gao X.
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Waste Powder Biotite as a Factor Enhancing the Flexural Strength of RPC. [PDF]
Grzeszczyk S +4 more
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Plagioclase feldspar is often surprisingly porous on a small scale. Pores range in size from less than 1 μm to about 40 μm, and occupy up to 2.3 % by volume. In general, the highest plagioclase porosities occur in rocks which would have had a comparatively “wet” history: normal granites and pegmatites.
Montgomery, Carla W., Brace, W. F.
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Partial Melting Reactions of Plagioclases and Plagioclase-Bearing Systems
1994The kinetics of partial melting were studied in the systems: $$\begin{gathered} \begin{array}{*{20}c} {Ab - An} & {{\text{ }}\left( {P = 1{\text{ }}atm} \right)} \\ \end{array} \hfill \\ \begin{array}{*{20}c} {Ab - An - H_2 O} & {{\text{ }}\left( {P = 5{\text{ }}kbar} \right)} \\ \end{array} \hfill \\ \begin{array}{*{20}c} {Qz - Ab - An - H_2 O} & {
W. Johannes, J. Koepke, H. Behrens
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