Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia

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Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia

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In West Anatolia near the cities of İzmir and Manisa, the historical occurrence of large earthquakes suggests the presence of important seismogenic faults. However, these faults have yet to be investigated in detail. The Manisa Fault Zone (MFZ) is an active large-scale normal fault system in this area, and thus field observations and palaeoseismological studies of this zone are important for predicting future earthquakes. | Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia

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Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia

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Đang chuẩn bị liên kết để tải về tài liệu: Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia

Basic Geological Mapping

Preliminary assessments of debris flow hazard in relation to geological environment changes in mountainous regions, North Vietnam

Needs of countries with longer timescale for deep geological repository implementation

Formation process of coastal ecoregions in relation to quaternary geological activities in Binh Thuan province

Geological values of lava caves in Krongno Volcano Geopark, Dak Nong, Vietnam

Geological controls on focused fluid flow in the Song Hong Basin, offshore Vietnam

Báo cáo "QUATERNARY GEOLOGICAL MAP OF THE CONTINENTAL SHELF OF VIETNAM AT THE SCALE OF 1:1,000,000 "

Evaluate the geological structure, petroleum potential by interpretation the 2D seismic data of Phu Quoc basina

Assessment of earthquake-induced ground liquefaction susceptibility for Hanoi city using geological and geomorphologic characteristics

Radiometric survey in geological mapping of parts of basement complex area of Nigeria

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Geological and palaeoseismological evidence for late Pleistocene−Holocene activity on the Manisa fault zone, Western Anatolia