نتایج جستجو برای: ultramafic rocks

تعداد نتایج: 22653  

Journal: :زمین شناسی اقتصادی 0
فریبرز خدادادی عبدالناصر فضل نیا حسین پیرخراطی

introduction heavy metals are the most toxic pollutants in aquatic ecosystems. this contamination can result from the release of heavy metal elements during alteration and weathering of ultramafic and mafic rocks (ophiolite zones). among the important metals and pollutants in the ophiolite; chromium, cobalt, nickel, iron, magnesium, manganese, zinc and copper could be noted. basically, a mass o...

Journal: :Open Journal of geology 2023

The Jayachamarajapura schist belt in western Dharwar craton, southern India, is predominantly an ultramafics dominant terrain. These rocks have been extensively metamorphosed and altered to serpentinite. komatiite nature of conspicuous. In most the areas these are massive nature. However, some ultramafic units show layered But, their outcrops encompassed within komatiitic bodies. Mg-rich also M...

2014
Marco Maffione Antony Morris Douwe J. J. van Hinsbergen

Serpentinization of ultramafic rocks during hydrothermal alteration at mid-ocean ridges profoundly changes the physical, chemical, rheological, and magnetic properties of the oceanic lithosphere. There is renewed interest in this process following the discovery of widespread exposures of serpentinized mantle on the seafloor in slow spreading oceans. Unroofing of mantle rocks in these settings i...

2017
Katrina I. Twing William J. Brazelton Michael D. Y. Kubo Alex J. Hyer Dawn Cardace Tori M. Hoehler Tom M. McCollom Matthew O. Schrenk

Serpentinization is a widespread geochemical process associated with aqueous alteration of ultramafic rocks that produces abundant reductants (H2 and CH4) for life to exploit, but also potentially challenging conditions, including high pH, limited availability of terminal electron acceptors, and low concentrations of inorganic carbon. As a consequence, past studies of serpentinites have reporte...

Journal: :The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists 1954

Journal: :Papers and Proceedings of The Royal Society of Tasmania 1983

یزدانی, مریم,

The Piranshahr ophiolitic complex is located in NW Iran, and at north west of the Piranshahr town. Tectonically, the NW Piranshahr ophiolitic complex is severely mélanged and the boundary of different units in this complex is undistinguishable. Piranshahr ophiolite includes ultramafic, mafic, sedimentary and metamorphic rocks. Mafic rocks with basalt and diabase compositions are exposed in seve...

نمودار تعداد نتایج جستجو در هر سال

با کلیک روی نمودار نتایج را به سال انتشار فیلتر کنید