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Determination of the P-T conditions and depths of magma storage zones for two distinct quaternary lava flows in the Southeast of Mount Ağrı (Eastern Anatolia, Turkey). [PDF]
Dogan-Kulahci GD.
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Editorial: Significance cytokines in immuno oncology and immunotherapy. [PDF]
Jurisic V.
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Physico-mechanical characterization and gamma radiation shielding capability of granodiorite from Suwayqat El-Arsha, Egypt; implications for construction and natural radiation shielding. [PDF]
Azer MK +4 more
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Dataset on thermophysical properties of natural stones for heat storage applications. [PDF]
Seyitini L, Belgasim B, Enweremadu CC.
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Contrasting mineralized and barren porphyries in the Zhongdian Arc, insights from biotite and apatite compositions and halogen fugacity. [PDF]
Pan Y +5 more
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Titanium in calcium amphibole: Behavior and thermometry
American Mineralogist, 2021Thermometry of high-grade metamorphic rocks is difficult due to fast cationic diffusion during slow cooling, but the titanium content of calcium amphibole (Ti-Amp) can retrieve amphibole-forming temperature as high as ~1000 °C.
Yue Liao, C. Wei, H. Rehman
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Inhalation Toxicology, 2022
Context: Though some significant advances have been made in recent decades to evaluate the importance of size and morphology (habit) of elongate mineral particles (EMPs), further research is needed to better understand the role of each dimensional metric
A. Korchevskiy, A. Wylie
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Context: Though some significant advances have been made in recent decades to evaluate the importance of size and morphology (habit) of elongate mineral particles (EMPs), further research is needed to better understand the role of each dimensional metric
A. Korchevskiy, A. Wylie
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American Mineralogist, 2021
Arc magmas, a major contributor to continental crust growth, are thought to be more oxidized than mid-ocean ridge basalts as reflected by an enrichment in ferric iron relative to ferrous iron. But how arc magmas become oxidized is hotly debated.
Jingbo Zhang, Rui Wang, Jun Hong
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Arc magmas, a major contributor to continental crust growth, are thought to be more oxidized than mid-ocean ridge basalts as reflected by an enrichment in ferric iron relative to ferrous iron. But how arc magmas become oxidized is hotly debated.
Jingbo Zhang, Rui Wang, Jun Hong
semanticscholar +1 more source

