نتایج جستجو برای: volcanic belt

تعداد نتایج: 31742  

Journal: :iranian journal of science and technology (sciences) 2015
m. rezaei

the kasian volcanic body is located in the eastern margin of the zagros thrust belt, close to the sanandaj-sirjan metamorphic zone. these volcanic rocks are mainly composed of andesite and andesite-basalt rocks with porphyritic, hypocrystalline porphyritic, hyalo-porphyritic and hyalo-microlitic porphyritic textures. analyses of the distributions of major, rare earth and trace elements reveal a...

2013
E. Chaussard F. Amelung Y. Aoki

[1] We use 2007–2011 Advanced Land Observing Satellite (ALOS) data to perform an arc-wide interferometric synthetic aperture radar (InSAR) time series survey of the Trans-Mexican Volcanic Belt (TMVB) and to study time-dependent ground deformation of four Indonesian volcanoes selected following the 2007–2009 study of Chaussard and Amelung (2012). Our objectives are to examine whether arc volcano...

2013
MICHAEL JAMES DELUCA

Wrangellia Superterrane. The Paleozoic to Mesozoic Wrangellia superterrane (Insular terrane) consists of intraoceanic volcanic assemblages and basement rocks of the Peninsular, Wrangellia, and Alexander terranes (Plafker et al, 1994). The magmatic-arc assemblages of the Peninsular terrane appear to have been built upon the Wrangellia composite terrane prior to the midCretaceous and include: 1) ...

2005
Sen Huy Tan

The Johanson Lake project is a two-year bedrock mapping program initiated by the Geological Survey and Development Branch in 2003 as part of the Toodoggone Targeted Geoscience Initiative (TGI). The project is focused on a belt of Mesozoic arc volcanic and plutonic rocks of the Quesnel Terrane in the eastern part of the McConnell Creek (94D) map sheet. This area contains a number of MINFILE occu...

Journal: :Science 2004
Harald Furnes Neil R Banerjee Karlis Muehlenbachs Hubert Staudigel Maarten de Wit

Pillow lava rims from the Mesoarchean Barberton Greenstone Belt in South Africa contain micrometer-scale mineralized tubes that provide evidence of submarine microbial activity during the early history of Earth. The tubes formed during microbial etching of glass along fractures, as seen in pillow lavas from recent oceanic crust. The margins of the tubes contain organic carbon, and many of the p...

Journal: :Zootaxa 2013
Ester H Oliveira Cristiano Lopes-Andrade

Cis taurus (Reitter) is the type-species of Macrocis Reitter, a genus subsequently synonymized with Cis Latreille. It names a diversified but barely studied species-group of Cis, the taurus group. The objective of the present work is to redescribe C. taurus, designate a lectotype and provide the first description of male abdominal terminalia of the species. We also provide new data on its geogr...

2003
NICHOLAS G. DIREEN ANTHONY J. CRAWFORD

Evidence for a c. 600 Ma rifted passive margin in eastern Australia exists in the form of multiple belts of mafic volcanic rocks preserved along the western margin of the Tasman Fold Belt System, and giving rise to elongate magnetic anomalies. Outcrop, drillhole and geophysical evidence points to piles of lavas, volcaniclastic and intrusive rocks up to 6 km thick, extending for strike lengths o...

احمدی‌پور, حمید , رحمانیان, زینب ,

The studied area is located about 35 KM north-west of Rafsanjan (Kerman Province) and belongs to Hezar volcanic complex (in Uromieh-Dokhtar volcanic belt) and consists of Eocene folded lava flows (basalt, basaltic andesite, andesite) and pyroclastic rocks. Plagioclase phenocrysts show evidences of disequilibrium textures such as sieve texture, resorption and oscillatory zoning. These features c...

Journal: :Philosophical transactions of the Royal Society of London. Series B, Biological sciences 2006
Frances Westall Cornel E J de Ronde Gordon Southam Nathalie Grassineau Maggy Colas Charles Cockell Helmut Lammer

Modelling suggests that the UV radiation environment of the early Earth, with DNA weighted irradiances of about three orders of magnitude greater than those at present, was hostile to life forms at the surface, unless they lived in specific protected habitats. However, we present empirical evidence that challenges this commonly held view. We describe a well-developed microbial mat that formed o...

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