Titlebook: Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes; Naci G?rür (President of Marmara Research Centre), Book 2

贊美

書目名稱Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes影響因子(影響力)




書目名稱Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes影響因子(影響力)學(xué)科排名




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書目名稱Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes被引頻次




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書目名稱Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes讀者反饋




書目名稱Integration of Earth Science Research on the Turkish and Greek 1999 Earthquakes讀者反饋學(xué)科排名

大量殺死

Imaging of the Izmit Rupture from the Strong Motion Records, Izmit earthquake. We find that rupture propagated at the sub-Rayleigh speed of about 3 km/s on the western and eastern segments of the fault, but that the central segment (Izmit — Sapanca Lake — Sakarya), nearly 50 km long, broke at the supershear speed of about 4.8 km/s. This value is, within the

兇猛

Tectonic Setting of the Eastern Marmara Sea, plays an important role on the tectonic evolution of the Marmara Sea region. On August 17, 1999, a devastating earthquake occurred on the northern strand of the North Anatolian Fault Zone with a M.=7.4 and struck the eastern Marmara Sea region. The main fault, which was well defined and mapped for

使長胖

Cpap155

外形

Methane in Sediments of the Deep Marmara Sea and Its Relation to Local Tectonic Structures,between the Tekirdag and the Central Marmara Basin is cut by a deep E-W-trending furrow which is the eastern branch of the Ganos Fault which in turn is part of the active North Anatolian Fracture Zone. This area was mapped during the Meteor cruise M 44/1 in February 1999. During the cruise seafloor

有害處

The Tsunami Threat in the Sea of Marmara, Turkey: A Review,may be the result of shaking from the next major earthquake or more probably, the secondary effect of sediment slumping on the seabed. This assessment is based on the extensive historical database available for the region and is supported by earthquake probability analysis, geological interpretation

glans-penis

上漲

The Athens Earthquake September 7, 1999 Neotectonic Regime and Geodynamic Phenomena, description of the morphotectonic evolution of the area affected by the earthquake is made. This attempt is based on observations concerning the general morphotectonic structure of Attica and on data concerning the geological — alpine and post-alpine — formations and structure. It is shown that the

adduction

Three-Dimensional P-Wave Crustal Velocity Structure beneath Athens Region (Greece) Using Micro-Earte a destructive earthquake of 5.9 Ms magnitude occurred on September 7, 1999. The investigated area is located at the eastern part of Greek mainland and was previously considered as a region of low seismicity. To investigate the 3-D crustal structure of the region a two-step tomography procedure has