نتایج جستجو برای: kouhbanan active fault zone

تعداد نتایج: 602840  

2002
Felix Waldhauser William L. Ellsworth

[1] The relationship between small-magnitude seismicity and large-scale crustal faulting along the Hayward Fault, California, is investigated using a double-difference (DD) earthquake location algorithm. We used the DD method to determine high-resolution hypocenter locations of the seismicity that occurred between 1967 and 1998. The DD technique incorporates catalog travel time data and relativ...

Journal: :Energies 2022

Field observations of active and fossil natural geothermal fields indicate that fluids are primarily transported along dikes fault zones. Fluid transport (commonly through fractures at their margins) is controlled by the cubic law where volumetric flow rate depends on aperture fracture in 3rd power. Dikes (and inclined sheets) also act as heat sources for fields. In high-temperature volcanoes I...

2005
WALTER J. ARABASZ

The Taltal area, which lies within the coastal cordillera of northern Chile, is dominated by a group of major active faults that cut a eugeosynclinal section of predominantly Jurassic andesites overlying Paleozoic metamorphic and plutonlc rocks and intruded by Late Mesozoic plutons. The Atacama fault, a suggested regional strike-sllp fracture parallel to the coastline, has been obliquely cut an...

Journal: :محیط شناسی 0
محمد رضا سمرقندی دانشگاه علوم پزشکی همدان، دانشیار گروه مهندسی بهداشت محیط دانشکدة بهداشت مهدی هادی دانشگاه علوم پزشکی کردستان ، مربی گروه مهندسی بهداشت محیط سعید عزیزیان دانشکاه بوعلی همدان ، استاد گروه شیمی-فیزیک دانشکدة شیمی مهری سلیمانی امین آباد دانشگاه علوم پزشکی کردستان ، دانشجوی کارشناسی ارشد مهندسی بهداشت محیط

the used activated carbon was derived from pine-cone and was used for the removal of acid black 1(ab1) and acid blue 113(ab113) dyes. a batch sorption study was carried out in order to obtain optimum isotherm model. the study showed the best fit of the adsorption isotherm data was obtained using the langmuir model for both dyes. the monolayer maximum saturation capacities of ab1 and ab113 dyes ...

2007
Christine A. Regalla David J. Anastasio Frank J. Pazzaglia

New geologic mapping, morphologic fault scarp modeling, and geomorphic metrics in the Red Rock Valley, southwestern Montana, help characterize the Quaternary history of the virtually unstudied Monument Hill fault and tectonics of the youthful and seismically active Red Rock graben. Two generations of Pleistocene surface ruptures are preserved along the Monument Hill fault. Similarity in rupture...

2011
William L. Ellsworth Peter E. Malin WILLIAM L. ELLSWORTH PETER E. MALIN

Damage to fault-zone rocks during fault slip results in the formation of a channel of low seismic-wave velocities. Within such channels guided seismic waves, denoted by Fg, can propagate. Here we show with core samples, well logs and Fg-waves that such a channel is crossed by the SAFOD (San Andreas Fault Observatory at Depth) borehole at a depth of 2.7 km near Parkfield, California, USA. This l...

Journal: :journal of sciences, islamic republic of iran 2011
h. hajialibeigi

the khushab anticline is located in the zagros fold-thrust belt in the lurestan. this anticline is affected by the balarud fault zone, which is a part of mountain front fault between the lurestan and dezful embayment zones. based on the measurement of the elements of fold style, this anticline is analyzed. according to these measurements, this anticline is a noncylindrical, asymmetrical and dis...

2012
Yihe Huang Jean-Paul Ampuero

The damaged rock around mature faults forms a zone of low seismic wave 24 velocities, which can perturb important earthquake rupture properties. In particular, waves 25 reflected within the fault zone structure can induce short-duration slip pulses, an apparently 26 predominant earthquake rupture mode. Another known mechanism to generate slip pulses is 27 strong velocity-weakening friction. Her...

2011
Gunnar Gunnarsson

Reinjection has posed a major problem in the operation of the Hellisheidi Power Plant, SWIceland. The formation temperature at the originally planned reinjection zone proved to be very hot (>300°C) when injection wells were drilled there. In order to be able to use that zone for production a new reinjection zone was planned. The new zone has been promising despite problems in operating the new ...

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