نتایج جستجو برای: source of magma

تعداد نتایج: 21186166  

2018
Corentin Caudron Robert S. White Robert G. Green Jennifer Woods Clare Donaldson Tim Greenfield Eleonora Rivalta Bryndís Brandsdóttir

Magma is transported in brittle rock through dikes and sills. This movement may be accompanied by the release of seismic energy that can be tracked from the Earth’s surface. Locating dikes and deciphering their dynamics is therefore of prime importance in understanding and potentially forecasting volcanic eruptions. The Seismic Amplitude Ratio Analysis (SARA) method aims to track melt propagati...

2000
James Brophy

Introduction In the following chapters we will find that nearly all of the varied aspects of volcanism are either directly or indirectly controlled by the chemical composition of magma and the rate at which it cools and solidifies. If you are to understand and appreciate subsequent discussions of volcanoes and related volcanic phenomena, it is essential that you have a good grasp of the basic c...

2003
Mark D. Behn John M. Sinton Robert S. Detrick

Studies along the Mid-Atlantic Ridge (MAR) and East Pacific Rise (EPR) show that seamount abundance is a strong function of spreading rate. At the MAR, small axial seamounts are a dominant morphologic feature of the inner valley floor, while at the EPR seamounts are rarely observed within the neovolcanic zone. The Gala¤pagos Spreading Center (GSC) provides an excellent location to test the infl...

2010
Burçin Eröcal William Stein

Sage is a free, open source, self-contained distribution of mathematical software, including a large library that provides a unified interface to the components of this distribution. This library also builds on the components of Sage to implement novel algorithms covering a broad range of mathematical functionality from algebraic combinatorics to number theory and arithmetic geometry.

Journal: :SIAM J. Discrete Math. 1993
Frank Ruskey Carla D. Savage

Let B be a basis of transpositions for Sn and let Cay B Sn be the Cayley graph of Sn with respect to B It was shown by Kompel makher and Liskovets that Cay B Sn is hamiltonian We extend this result as follows Note that ev ery transposition b in B induces a perfect matchingMb in Cay B Sn We show here when n that for any b B there is a Hamilton cycle in Cay B Sn which includes every edge of Mb Th...

2006
Paul Lundgren Zhong Lu

[1] We analyzed RADARSAT-1 synthetic aperture radar (SAR) data to compute interferometric SAR (InSAR) images of surface deformation at Uzon caldera, Kamchatka, Russia. From 2000 to 2003 approximately 0.15 m of inflation occurred at Uzon caldera, extending beneath adjacent Kikhpinych volcano. This contrasts with InSAR data showing no significant deformation during either the 1999 to 2000, or 200...

تنها , علی, خانعلی زاده, علیرضا , صادقیان, محمود , قاسمی, حبیب ا.. ,

Neogene high silica adakitic domes of south Quchan, cropped out in the northern part of the Quchan-Esfarayen Cenozoic magmatic arc (north of Sabzevar ophiolitic and metamorphic belt). In this volcanic belt, magmatic activities has been started since Eocene (about 40 Ma ago) and continued to Plio-Pleistocene (about 2 Ma ago). The ages of volcanic rocks range from Eocene to Plio-Pleistocene from ...

احمدی مقدم, پریچهر, احمدی پور, حمید, مرتضوی, محسن, پوستی, محمد,

The Hormuz Formation is a sequence of lithologically various evaporitic–volcanic rocks in salt domes where the volcanic rocks are dominantly acidic, generally with less than one third basic volcanics. It was formed in the Late Proterozoic (640–620 Ma)/Neoproterozoic–Early Cambrian, as a result of sub-basin rifting in the northern part of the Arabian plate, throughout most of the Persian Gulf Ba...

Asiabanha, Abbas, Ebrahimi, Mohammad, Emadi, Fatemeh,

The Kahrizbeyg pluton is located northwest of Iran in Central Iran zone. It is emplaced into the Cretaceous limestones in which contact metamorphism has happened. Meanwhile, rock fragments of this pluton are found in conglomerate units of Early Oligocene Lower Red Formation. Therefore, the relative age of pluton is between Cretaceous and Oligocene. The Kahrizbeyg pluton consists of granite and ...

ارجمندزاده, رضا, الماسی, علیرضا, فرانسیسکو سانتوز, ژوزه, کریم‌پور, محمدحسن,

On the basis of field studies, mafic-intermediate bodies of Kashmar are subdivided into the old series (often stocks of gabbro, diorite, quartz diorite/monzodiorite) and the new series (quartz monzodiorite swarm dykes). In terms of crosscutting relationships, old series has the age between oldest volcanic units (57 Ma) and Eocene granitoids (40 Ma), but the swarm dykes are attributed to the pos...

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