Results 41 to 50 of about 1,786 (213)
Determination of Lu and Hf Mass Fractions and
Qian Ma, Yue‐Heng Yang, Zhiming Yang
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Baula and Pomalaa Ophiolitic Complexes are part of East Sulawesi Ophiolite (ESO). The ultramafic rocks in the Baula and Pomalaa Ophiolite Complex mainly is peridotite and consist of harzburgite, lherzolite and olivine websterite, mostly serpentinized ...
Rio Irhan Mais Cendrajaya +7 more
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The Kylmäkoski nickel-copper deposit in south-western Finland [PDF]
The Kylmäkoski sulfide Ni-Cu deposit is located in southwestern Finland in the WNW trending Pori-Kylmäkoski nickel belt which contains several other sulfide Ni-Cu occurrences besides Kylmäkoski. The original reserves of the Kylmäkoski ore were ca.
H. Papunen
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Origin of magnetic fabrics in ultramafic rocks [PDF]
IOP Conference Series: Materials Science and Engineering, 82 (1)
Biedermann A.R. +3 more
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This study evaluates the impact of mineralogy, elemental composition, and reaction pathways on hydrogen (H2) generation in seven ultramafic and mafic (basaltic) rocks. Experiments were conducted under typical low-temperature hydrothermal conditions (150 °
Abubakar Isah +2 more
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Mineral chemistry and petrological implications of rock-forming minerals from Permian mafic-ultramafic intrusions in the Gansu-Xinjiang Beishan area [PDF]
Bocheng MA +7 more
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DOI: 10.17014/ijog.5.3.277-290The North Konawe Regency, located in the northern part of the southeast arm of Sulawesi Province, is occupied mainly by Ophiolite Complex.
Ronaldo Irzon, Baharuddin Abdullah
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The Bhavani Suture Zone, a region in the Southern Granulite Terrane (SGT), is where the Neoarchean Madurai Block and the Southern Madurai Block in western Tamil Nadu have been joined.
M. Monisha, M. Muthukumar, V.J. Rajesh
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Quantifying Natural Hydrogen Generation Rates and Volumetric Potential in Onshore Serpentinization
This study explores the generation of natural hydrogen through the serpentinization of onshore ultramafic rocks, highlighting its potential as a clean energy resource.
Reza Rezaee
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The paper presents the geochemistry, origin and geodynamic setting of podiform chromitite and host rocks from the Buem Structural Unit (BSU) in the northwestern Benin Republic.
Daniel N. Kouagou N’Dah +7 more
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