منابع مشابه
Effects of serpentinization degree on the geotechnical characteristics of ultramafic rocks in the southwest of Mashhad city (Iran)
The present work was conducted to investigate the geotechnical properties of two meta-peridotites and meta-pyroxenites of an ultramafic complex mainly consisting of ultramafic rocks. For this purpose, microscopic studies were performed to determine the percentage of serpentinization in these rocks. In addition, a number of mechanical and physical tests were performed on collected samples with d...
متن کاملMineralogy Determinations by Chemin Xrd, Tested on Ultramafic Rocks
across) and UI-21 (1.5 cm across). UI-3 is a websterite, composed of augite (gray), orthopyroxene (white) and spinel (brown); at the top is the host basalt. UI-21 is a spinel lherzolite; spinel is brown, other phases near-white. MINERALOGY DETERMINATIONS BY CHEMIN XRD, TESTED ON ULTRAMAFIC ROCKS (MANTLE XENOLITHS). A. H. Treiman, K. L. Robinson, D. F. Blake, and D. Bish. Lunar and Planetary Ins...
متن کاملResolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean
Airborne transport of microbes may play a central role in microbial dispersal, the maintenance of diversity in aquatic systems and in meteorological processes such as cloud formation. Yet, there is almost no information about the abundance and fate of microbes over the oceans, which cover >70% of the Earth's surface and are the likely source and final destination of a large fraction of airborne...
متن کاملCorrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean
[This corrects the article on p. 557 in vol. 5, PMID: 25400625.].
متن کاملGeological Carbon Capture & Storage in Mafic and Ultramafic Rocks Geological Carbon Capture and Storage in Mafic and Ultramafic Rocks – Muscat, 2011
1 Geological carbon capture and storage in mafic and ultramafic rocks – Muscat, 2011
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ژورنال
عنوان ژورنال: Geophysical Journal International
سال: 2001
ISSN: 0956-540X,1365-246X
DOI: 10.1046/j.0956-540x.2000.01280.x