Hyperalgesia
发表于 2025-3-27 00:30:06
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CAMP
发表于 2025-3-27 04:44:36
1568-1238 Düzce and Athens earthquakes and assesses the data that are available and relevant to the geology, seismology, tectonics, geodesy and other fields related to earthquake studies and to evaluate earthquake hazard potential.978-1-4020-0654-8978-94-010-0383-4Series ISSN 1568-1238
英寸
发表于 2025-3-27 09:17:48
,The 17 August 1999 Gölcük (Kocaelı)- Arıfıye (Adapazari) and 12 November 1999 Düzce Earthquakes, NWe east of Gölcük-Arifiye line and created a 38 km long surface rupture. The maximum rigth-lateral displacement of 4.5 m occurred in the middle of the surface rupture. To the south of Düzce, the surface ruptures of two earthquakes overlapped by about 10 km length. Düzce earthquake must have been triggered by Gölcük-Arifiye earthquake.
Introduction
发表于 2025-3-27 11:16:34
Imaging of the Izmit Rupture from the Strong Motion Records,sula over about 30 km while it stopped abruptly at depth at the termination of the eastern (Karadere) segment. The slip duration is between 2 and 4 s except in the hypocentral area that slipped in about 1 s. The seismic moment inferred is about 2.5 × 10. N·m.
DEFT
发表于 2025-3-27 14:32:14
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receptors
发表于 2025-3-27 18:26:23
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HILAR
发表于 2025-3-28 01:58:50
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取之不竭
发表于 2025-3-28 02:21:00
Methane in Sediments of the Deep Marmara Sea and Its Relation to Local Tectonic Structures,rs where methane is oxidized to H. and CO.; the H. reduces the sulfate that finally is converted to H.S. This H.S forms iron-sulfide precipitates in the presence of reduced iron. However, our geochemical concentration profiles are not typical for steady-state conditions, but are rather characterized
adulterant
发表于 2025-3-28 09:45:41
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责任
发表于 2025-3-28 10:55:48
Three-Dimensional P-Wave Crustal Velocity Structure beneath Athens Region (Greece) Using Micro-Eartedominant in the investigated region, without any sharp horizontal velocity variation. The low velocities at this depth seem to be typical for sedimentary basins, like those of the investigated region. The most predominant feature is a low velocity layer at a depth of 6—8 km. At the same depth, few