Results 31 to 40 of about 1,173 (159)
(1) Background: Microbial communities in terrestrial, calcifying high-alkaline springs are not well understood. In this study, we investigate the structure and composition of microbial mats in ultrabasic (pH 10–12) serpentinite springs of the Voltri ...
Aysha Kamran +5 more
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Fluid‐Mediated Mass Transfer Between Mafic and Ultramafic Rocks in Subduction Zones
Metasomatic reaction zones between mafic and ultramafic rocks exhumed from subduction zones provide a window into mass‐transfer processes at high pressure.
E. A. Codillo +6 more
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The serpentinite samples of the Prang Ghar Mohmand Agency were analysed petrographically and physicomechanically to assess their potential as dimension stone and aggregate material.
M. Naveed Anjum +4 more
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Serpentinized peridotite samples—considered nowadays as deposited waste at the magnesite mine of Gerakini (Chalkidiki, N. Greece)—were collected, and their chemical and mineralogical characterization analyzed with Energy-Dispersive X-ray Fluorescence (ED-
Dimitra Papargyriou +5 more
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Application of the shrinking core model for dissolution of serpentinite in an acid solution
Serpentinites have the potential to be used as carbo dioxide capture and storage materials. Acid dissolution is the first stage of this process. This study examined how a shrinking core model can be applied to the dissolution of serpentinite in sulphuric
Didyk-Mucha Agnieszka +2 more
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: Lichi mélange, located in the southern coastal range, eastern Taiwan, China, is a typical tectonic mélange of the plate’s boundary zone between the Eurasian Plate and the Philippine Sea Plate.
Long Huang, Wei Geng, Zhi-lei Sun
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Tracking Subsurface Active Weathering Processes in Serpentinite
We conducted a novel study to capture the on‐going advancement of mineral weathering within a serpentinite formation by using an integrated approach of multi‐scale quantitative rock magnetic analyses and nano‐resolution geochemical imaging analyses.
Masako Tominaga +7 more
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This study conducts low-vacuum sulfidation to form a sulfidation layer on the serpentinite-derived magnesium iron silicate, thereby enhancing its electrochemical properties. Results show (Mg,Fe)2SiO4 calcined at 900 °C has the best crystallinity, and the
Jun-Ren Zhao +4 more
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We present the geological map (1:10.000) of the Montecastelli Pisano area, where (i) the relationships between Neogene-Quaternary transfer and normal faults have been carefully mapped (Sheet 1), and (ii) the mantle sequence of the Ligurian Ocean has been
Andrea Brogi +3 more
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Dynamic earthquake rupture preserved in a creeping serpentinite shear zone
Creeping serpentinite shear zones may host large earthquakes, but direct evidence of frictional heating and rupture have been missing. Here, the authors demonstrate via laboratory experiments that earthquake ruptures can propagate through serpentinite ...
Matthew S. Tarling +3 more
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