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Mineral inclusions under non-ambient conditions

Mineral inclusions represent a real treasure in earth sciences because of their large range of applicability to unravel metamorphic and geodynamic processes. For instance, the contrast in the thermal expansion and compressibility coefficients between a mineral inclusion and its surrounding host leads to a residual pressure in the inclusion (Pinc) that,
Nicola Campomenosi   +3 more
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Rounded mineral inclusions in upper mantle peridotite

Physics of the Earth and Planetary Interiors, 1981
Abstract Mantle-derived peridotite xenoliths contain abundant olivine with rounded spinel and orthopyroxene inclusions, and orthopyroxene with rounded olivine and spinel inclusions. The shape-change of spinel, olivine and orthopyroxene inclusions from the primarily polyhedral outline to the spherical outline is governed by interfacial diffusion of ...
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Application of fluid inclusions in mineral exploration

Journal of Geochemical Exploration, 1991
Abstract Fluid inclusions provide information on the genesis of mineral deposits and can be used in mineral exploration. A hidden orebody at the Sangdong tungsten ore deposit was found by fluid inclusion study. Maximum homogenization temperature values obtained from quartz in skarn at Sangdong delineated the main channel of ore fluid, as well as ...
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Mineral fluid inclusions

2020
Shuming Wen, Jian Liu, Jiushuai Deng
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Internal composition of mineral fluid inclusions

2021
Shuming Wen, Jian Liu, Jiushuai Deng
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Effects of Palygorskite Inclusion on the Growth Performance, Meat Quality, Antioxidant Ability, and Mineral Element Content of Broilers

Biological Trace Element Research, 2016
Yefei Cheng   +5 more
semanticscholar   +1 more source

Dynamic interactions at the mineral–organic matter interface

Nature Reviews Earth & Environment, 2021
Markus Kleber   +2 more
exaly  

Systematics of Fluid Inclusions in Diagenetic Minerals

1994
The past decade has revealed significant advantages to using fluid inclusions as a means of understanding the physical and chemical history of fluids in sedimentary basins, but it also has revealed important limitations which have required that a new approach must be employed to effectively use fluid inclusions. This book is divided into six sections: (
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