نتایج جستجو برای: clay alteration

تعداد نتایج: 67160  

2014
Tariq Siddique Petr Kuznetsov Alsu Kuznetsova Nicholas Arkell Rozlyn Young Carmen Li Selma Guigard Eleisha Underwood Julia M. Foght

Dispersed clay particles in mine tailings and soft sediments remain suspended for decades, hindering consolidation and challenging effective management of these aqueous slurries. Current geotechnical engineering models of self-weight consolidation of tailings do not consider microbial contribution to sediment behavior, however, here we show that microorganisms indigenous to oil sands tailings c...

Abbasnia, Hosain, Karimpour, Mohammadhasan, Malekzadeh Shafaroudi, Azadeh,

The Damanghor gold mineralization occurrence is located in north of Bardaskan, Khorasan Razavi Province, and Taknar zone.The geology of the area consists of Precambrian green sericite schist and metarhyolite, intruded by diabase. Mineralization in this area is in vein form with N50E stribe and 70NW dip and hosted by schist and metarhyolite with 300 meters length and 2 to 35 meters width. Dissem...

1984
R. R. ANAND

-In a lateritic pallid zone ilmenite crystals alter via pseudorutile to porous leucoxene grains composed of randomly oriented aggregates of ~0.06/~m anatase crystals. This style of alteration differs from that in beach sands where parallel oriented futile crystals develop from pseudorutile. Increased Si and A1 in the altered grains is due to the crystallization from soil solution of halloysite,...

2013
Janice L. Bishop Damien Loizeau Nancy K. McKeown Lee Saper M. Darby Dyar David J. Des Marais Mario Parente Scott L. Murchie

Phyllosilicate deposits on Mars provide an opportunity to evaluate aqueous activity and the possibility that habitable environments may have existed during the Noachian period there. Analysis of hyperspectral visible/near-infrared (VNIR) Mars Reconnaissance Orbiter (MRO) Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) images has shown thick, complex profiles of phyllosilicates at M...

جهانگیری, احمد, سیمونز, وارطان, موید, محسن, کلاگری, علی اصغر ,

Quartz-monzonitic porphyry stock at Kighal is located about 12 km north of Varzeghan, East Azarbaidjan Province, NW Iran. It has intruded older volcanic units during magmatic activities of Pyrenean orogenic phase and produced Cu-Mo mineralization and hydrothermal alteration zones in the region. The stock was intruded by numerous cross-cutting dikes mainly of dioritic to quartz-dioritic composit...

Journal: :Journal Of Geophysical Research: Planets 2022

Glen Torridon (GT) is a recessive-trough feature on the northwestern slope of “Mt. Sharp” in Gale crater, Mars with highest Fe-/Mg-phyllosilicates abundances detected by Curiosity rover to date. Understanding origin these clay minerals and their relationship diagenetic processes critical for reconstructing nature habitability past surface subsurface environments crater. We aim constrain distrib...

2017
Mary Anne Holmes

The early opening of the South Atlantic ocean along the eastern Romanche Fracture Zone, including an initial phase of transform faulting and pull-apart basin formation, followed by the generation of a seafloor spreading center, was investigated during Ocean Drilling Program Leg 159 to the Côte d’Ivoire-Ghana continental margin. Clay minerals in the <0.5-μm fraction of tectonically disturbed sed...

Journal: :Journal of Petroleum Exploration and Production Technology 2022

Abstract The well NSE-001 is an exploration located in the North Sumatra Basin, Indonesia, which penetrates several formations with overpressure zones that have potential as a drilling hazard this area. results of pore pressure fracture gradient model show response wireline log data based on normal compaction trend has two types mechanisms, namely loading and unloading. Rapid sedimentation deve...

اعتمادی, بیژن, تقی‌پور, بتول, قبادی, عبدالهادی,

Nodoushan clay deposit is located about 130km southwest of Yazd city in the Uromieh-Dokhtar volcano-plutonic belt. Based on the field, mineralogical and geochemical studies, the rocks of Nodoushan area are of volcanic type and are composed of dacite, andesite and olivine-basalt, the pyroclastic type (crystalline tuff), and the microgranodioritic intrusive rocks. According to Zr/TiO2 versus SiO2...

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