A rapid transition from subduction to Barrovian metamorphism: geochronology of mafic-ultramafic relicts of oceanic crust in the Central Alps, Switzerland. [PDF]
Swiss J GeosciLemke K, Rubatto D, Hermann J.
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A geophysical investigation of the fairy circles in Nebraska for geologic hydrogen exploration. [PDF]
Sci RepZhang M +4 more
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Insight into drilling performance parameters for in-situ detection of lithological transition. [PDF]
Sci RepTanimoto K, Hamada Y, Katayama I.
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Characterization, Source Analysis, and Ecological Risk Assessment of Heavy Metal Pollution in Surface Soils from the Central-Western Ali Region on the Tibetan Plateau. [PDF]
ToxicsHuang Y, He T, Luo J, Ma X, Zhang T.
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A Paleoarchaean impact crater in the Pilbara Craton, Western Australia. [PDF]
Nat CommunKirkland CL +6 more
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Trench sediment heterogeneity controls accretion mechanisms in subduction zone. [PDF]
Sci RepSanità E +5 more
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Structures control gold mineralization in the western Allaqi shear belt of Egypt from high-precision geophysical and remote sensing datasets. [PDF]
Sci RepEldosouky AM +3 more
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Peridotites and other ultramafic rocks
Geology TodayPeridotites are a group within the category of ultramafic rocks. These are usually dark‐coloured rocks rich in magnesium, poor in silica and lacking feldspars. Earth's mantle, which makes up 83 percent by volume and 67 percent by weight of the planet, consists largely of peridotite, which, although relatively sparse at the surface, therefore, is Earth ...
Kent Brooks
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