نتایج جستجو برای: rock alteration

تعداد نتایج: 83344  

2006
D. W. Ming D. W. Mittlefehldt R. V. Morris D. C. Golden R. Gellert A. Yen B. C. Clark S. W. Squyres W. H. Farrand S. W. Ruff R. E. Arvidson G. Klingelhöfer H. Y. McSween D. S. Rodionov C. Schröder P. A. de Souza A. Wang

[1] Water played a major role in the formation and alteration of rocks and soils in the Columbia Hills. The extent of alteration ranges from moderate to extensive. Five distinct rock compositional classes were identified; the order for degree of alteration is Watchtower ffi Clovis > Wishstone ffi Peace > Backstay. The rover’s wheels uncovered one unusual soil (Paso Robles) that is the most S-ri...

2012
Jiping Wang Hongxia Liu Bo Chen Qiang Li Xuliang Huang Liqun Wang Xiaohua Guo Qiaobing Huang

BACKGROUND The role of advanced glycation end products (AGEs) in the development of diabetes, especially diabetic complications, has been emphasized in many reports. Accumulation of AGEs in the vasculature triggers a series of morphological and functional changes in endothelial cells (ECs) and induces an increase of endothelial permeability. This study was to investigate the involvement of RhoA...

Journal: :Applied sciences 2022

The sandstones which constitute the host rock for prehistoric artwork in Rock Groups of Tajo de las Figuras and Peñas Cabrera (southern Spain) show a serious degree alteration, due both to natural processes those related anthropogenic animal activity. A detailed study was carried out on petrological compositional characteristics (fresh altered rock) groups, geological climatological area they a...

پایان نامه :وزارت علوم، تحقیقات و فناوری - دانشگاه فردوسی مشهد - دانشکده علوم 1376

saluk mount is selected for devonian biostratigraphy. this area located at southwest of bojnurd. in this study three sections are selected and two sections, chahar-borj and tabar sections with a thickness of 650 m, which consist mainly of calcareous sediments was studied in detailed but third section, qelli section, with a thickness of about 450m which consist mainly of sandstone and evaporates...

کریم‌پور, محمدحسن, ابراهیمی, خسرو , زیرجانی‌زاده, صدیقه ,

The study area (Kalateh-No) is located in NW of Gonabad city in Khorasan Razavi Province. This area is located in geotectonic Lut Block zone. The rock types are mainly of volcanic and subvolcanics. The most important alteration zones are silisification, propylitic, argillic, serisitic and quartz-serisit-pyrite. The mineralizations have formed by intrusion of hydrothermal fluids of monzodiorite ...

Journal: :زمین شناسی اقتصادی 0
علی امامعلی پور مستوره یوسفی مهدیه کریملو

alteration of ophiolitic ultramafic rocks, formation of listwaenite and associated mineralization are interesting phenomena of metallogeny of khoy ophiolite. it seems that the hydrothermal circulations responsible for mercury mineralization were derived from geothermal systems caused by intermediate to acidic magmatism in neogene-pleistocene time. reactivation of brecciated serpentinite with hy...

Journal: :Chemical Geology 2021

Hypogene speleogenesis involves the formation of solution-enlarged permeability structures driven by ascending water acquiring its acidity from deep-seated sources. This process occurs in a wide range geological settings and different lithologies. Although hypogene has received increasing attention last two decades, identification former activity caves remains challenging, unless unambiguous mo...

رحیمی, بهنام, ملک‌زاده شفارودی, آزاده, کریمی سعیدآبادی, زهرا, کریم‌پور, محمدحسن,

Kariro Pb prospect area, which is located in northwest of Boshruyeh, occurs as vein-veinlets, open space filling, and cement of fault breccia in Middle Jurassic metamorphosed shale (slate) unit of Baghamshah Formation. Mineralization zones contain dolomite (70-85%) and galena (0.5-2.5%) with small amounts of pyrite, quartz, and calcite. Dolomitization and silicification of host rock are the mos...

اعتمادی, بیژن , میری, روح ا… ,

Fire clay of the Kabutarkuh deposit, located about 50 km southeast of Gonabad (Khorasan Province), was analyzed for its mineralogical and chemical compositions. Kaolinite, pyrophilite, quartz, dickite, gypsum, illite and alunite are the dominant minerals, and a minor phase of hematite is also present. Geochemical data show that the whole rock sample is mainly composed of SiO2, Al2O3 and K2O. Ch...

Journal: :NHM 2010
Steinar Evje Aksel Hiorth

Previous experimental studies of spontaneous imbibition on chalk core plugs have shown that seawater may change the wettability in the direction of more water-wet conditions in chalk reservoirs. One possible explanation for this wettability alteration is that various ions in the water phase (sulphate, calcium, magnesium, etc.) enter the formation water due to molecular diffusion. This creates a...

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