نتایج جستجو برای: hydrothermal fluids

تعداد نتایج: 59909  

تقی پور, بتول ,

Torud-Chah Shirine magmatic arc is located in south of Semnan. This arc is composed of Cenozoic volcanic, pyroclastic and intrusive rocks. The Kuh-Zar in manning province of Bagho is outstanding with Cu-Au mineralization. Mining is restricted to hydrothermal alteration zones in the area. Alteration zones includes propylitic, phyllic, advanced argillic and silicic. The rare association of tourma...

علی آبادی, محمدعلی, پورکاسب, هوشنگ, زراسوندی, علیرضا , طاهری, صادق ,

The Robat-Paein barite deposit is located about 30 Km northwest of Khomein city, in the Sanandajـ Sirjan zone. The Lower Cretaceous carbonate sequences are the host rock of barite mineralization in the Robat-Paein­ deposit.­­ These carbonate sequences consist mainly of massive bedded orbitolina-bearing limestone (undergone dolomitization in some areas) as well as marl, shale and thinly bedded l...

2008
Vesselin Dekov Jan Scholten Carl-Dieter Garbe-Schönberg Reiner Botz Javier Cuadros Mark Schmidt Peter Stoffers

[1] An active seafloor hydrothermal system subjects the background sediments of the Grimsey Graben (Tjörnes Fracture Zone) to alteration that produces dissolution of the primary volcaniclastic matrix and replacement/precipitation of sulfides, sulfates, oxides, oxyhydroxides, carbonates and phyllosilicates. Three types of hydrothermal alteration of the sediment are defined on the basis of the do...

2018
Lisa Richter Larryn W. Diamond Petya Atanasova David A. Banks Jens Gutzmer

Most rare earth element deposits form from magmatic fluids, but there have also been discoveries of heavy rare earth element (HREE)– enriched hydrothermal xenotime deposits within sedimentary basins. As xenotime is notoriously insoluble, the question arises as to whether these lesser-known deposits form at typical basin temperatures or by influx of much hotter magmatic-hydrothermal fluids. The ...

2018
F. Westall K. Hickman-Lewis N. Hinman P. Gautret K.A. Campbell J.G. Bréhéret F. Foucher A. Hubert S. Sorieul A.V. Dass T.P. Kee T. Georgelin A. Brack

Critical to the origin of life are the ingredients of life, of course, but also the physical and chemical conditions in which prebiotic chemical reactions can take place. These factors place constraints on the types of Hadean environment in which life could have emerged. Many locations, ranging from hydrothermal vents and pumice rafts, through volcanic-hosted splash pools to continental springs...

Journal: :زمین شناسی اقتصادی 0
فروغ ملک محمودی محمود خلیلی

introduction agates are presumed as a kind of precious stone that could be formed in magmatic, metamorphic and even sedimentary environment. mechanism for agate formation is not clear and is produced in laboratories. some hot springs and geothermal activity or white chimneys in the ocean floor, have some deposits like chalcedony but never produce agate. agate formation temperature varies betwee...

2012
Douglas P. Connelly Jonathan T. Copley Bramley J. Murton Kate Stansfield Paul A. Tyler Christopher R. German Cindy L. Van Dover Diva Amon Maaten Furlong Nancy Grindlay Nicholas Hayman Veit Hühnerbach Maria Judge Tim Le Bas Stephen McPhail Alexandra Meier Ko-ichi Nakamura Verity Nye Miles Pebody Rolf B. Pedersen Sophie Plouviez Carla Sands Roger C. Searle Peter Stevenson Sarah Taws Sally Wilcox

The Mid-Cayman spreading centre is an ultraslow-spreading ridge in the Caribbean Sea. Its extreme depth and geographic isolation from other mid-ocean ridges offer insights into the effects of pressure on hydrothermal venting, and the biogeography of vent fauna. Here we report the discovery of two hydrothermal vent fields on the Mid-Cayman spreading centre. The Von Damm Vent Field is located on ...

Journal: :Geochemical Transactions 2008
Heileen Hsu-Kim Katherine M Mullaugh Jeffrey J Tsang Mustafa Yucel George W Luther

BACKGROUND The speciation of dissolved sulfide in the water immediately surrounding deep-ocean hydrothermal vents is critical to chemoautotrophic organisms that are the primary producers of these ecosystems. The objective of this research was to identify the role of Zn and Fe for controlling the speciation of sulfide in the hydrothermal vent fields at the Eastern Lau Spreading Center (ELSC) in ...

2006
Giora Proskurowski Marvin D. Lilley Deborah S. Kelley Eric J. Olson

Although commonly utilized in continental geothermal work, the water–hydrogen and methane–hydrogen isotope geothermometers have been neglected in hydrothermal studies. Here we report δD-CH4 and δD-H2 values from high-temperature, black smoker-type hydrothermal vents and low-temperature carbonate-hosted samples from the recently discovered Lost City Hydrothermal Field. Methane deuterium content ...

2017
Nicholas R. J. Goodwin Ray Burgess Dave Craw Damon A. H. Teagle Chris J. Ballentine

The world-class Macraes orogenic gold deposit (∼10Moz resource) formed during the late metamorphic uplift of a metasedimentary schist belt in southern New Zealand. Mineralising fluids, metals and metalloids were derived from within the metasedimentary host. Helium and argon extracted from fluid inclusions in sulphide mineral grains (three crush extractions from one sample) have crustal signatur...

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