Results 121 to 130 of about 1,105,251 (141)
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Applied Geochemistry, 2002
Abstract Quartz crystals from mineralised joints of the Carpathian flysch contain fluid inclusions covering the compositional range from gaseous CH4±CO2±C2+ mixture, through CH4-saturated oil, to CH4-saturated aqueous solution. The C isotope composition of CH4 extracted from the fluid inclusions (−31 and −36‰ V-PDB) is indicative of a thermogenic dry
Vratislav Hurai +4 more
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Abstract Quartz crystals from mineralised joints of the Carpathian flysch contain fluid inclusions covering the compositional range from gaseous CH4±CO2±C2+ mixture, through CH4-saturated oil, to CH4-saturated aqueous solution. The C isotope composition of CH4 extracted from the fluid inclusions (−31 and −36‰ V-PDB) is indicative of a thermogenic dry
Vratislav Hurai +4 more
openaire +1 more source
The Western Azerbaijan Ophiolite (NW Iran): Evidence for Magmatic Evolution in a Fore-arc Basin
Zagros ophiolites represent remnants of the Neo-Tethyan Ocean, which are distributed within the Alpine-Himalayan orogenic belt. The Dalampar ophiolitic mélange is a part of the Late Cretaceous Zagros ophiolitic belt located in western Azerbaijan, close to the borders of Turkey and Iraq.Ayoub Veisinia +7 more
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Tertiary Tectonics and Sedimentation in the Salin (Fore-Arc) Basin, Myanmar
AAPG Bulletin, 1991openaire +1 more source
Geology and Petroleum Potential of the Indonesian Fore-Arc Basins: ABSTRACT
AAPG Bulletin, 1990openaire +1 more source
Sedimentary development of the Tertiary fore‐arc basin in southwestern Nicaragua, Central America
GFF, 1996R.A. Kumpulainen +5 more
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Structural Influences on Neogene Subsidence in the Central Sumatra Fore-Arc Basin
1992Richard G. Matson, Gregory F. Moore
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Cainozoic Basin-Forming Tectonism in the Southern Fore-Arc Zone of Sumatra
AAPG Bulletin, 1992openaire +1 more source