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The Dihedral Angle and Intersection Processes of a Conjugate Strike-Slip Fault System in the Tarim Basin, NW China
Conjugate fault strike-slip dihedral angle fault intersection faulting process Carbonate
2018/4/10
Recent studies, focused on dihedral angles and intersection processes, have increased understandings of conjugate fault mechanisms. We present new 3-D seismic data and microstructural core analysis in...
Paleoseismology of silent faults in the Central Apennines (Italy):the Campo Imperatore Fault (Gran Sasso Range Fault System)
paleoseismology active fault Holocene Central Italy
2015/9/16
Paleoseismological analyses were performed along the Campo Imperatore Fault (part of the Gran Sasso Range Fault System) in order to define the seismogenic behaviour (recurrence interval for surface fa...
Shallow to intermediate resistivity features of the Colfiorito Fault System inferred by DC and MT survey
Colfiorito fault system magnetotellurics geoelectrics fluids
2015/9/1
Over the last decade electromagnetic (EM) measurements have provided new constraints on the upper-crustal structure of the major fault zones in the world, both when they act as conduit and as a barrie...
Truthfulness of the Existence of the Pelusium Megashear Fault System, East of Cairo, Egypt
Pelusium Megashear Fault Hazard Recurrence Cairo
2013/3/11
The so-called Pelusium Megashear System (PMS), consists of echelon left-lateral megashears crossing Africa from the Nile-Delta since the Precambrian times. Although this system is questioned by some s...
Displacements and Kinematics of the February 1, 1944 Gerede Earthquake (North Anatolian Fault System, Turkey): Geodetic and Geological Constraints
North Anatolian Fault System Gerede fault zone Gerede earthquake coseismic deformation GPS triangulation
2010/10/14
The North Anatolian Fault System (NAFS) is an approximately 2-110-km-wide, 1600-km-long right-lateral intra-continental transform fault boundary between the Anatolian platelet and the Eurasian plate. ...
The June 6, 2000, Orta (Çankırı, Turkey) Earthquake: Sourced from a New Antithetic Sinistral Strike-slip Structure of the North Anatolian Fault System, the Dodurga Fault Zone
North Anatolian Fault System Antithetic Fault Sinistral Strike-slip Fault Orta Earthquake
2009/7/8
The İsmetpaşa-Kargı section of the North Anatolian Fault System (NAFS) consists of six subfault zones, namely the Eskipazar, the Ulusu, the Tosya, the Çerkeş-Kurşunlu, ...
Timing of Late Holocene Earthquakes on the Eastern Düzce Fault and Implications for Slip Transfer between the Southern and Northern Strands of the North Anatolian Fault System, Bolu, Turkey
North Anatolian Fault System slip transfer active fault palaeoseismology Holocene
2009/7/8
Results of trenching across the eastern Düzce Fault document that surface rupture has occurred repeatedly on the fault prior to the 1999 Düzce earthquake, and that offset during previous earthquakes ...
Different Modes of Stress Transfer in a Strike-slip Fault Zone: an Example From the North Anatolian Fault System in Turkey
North Anatolian Fault System (NAFS) strike-slip faulting earthquake stress transfer
2009/7/7
The dextral North Anatolian Fault System (NAFS) extends for well over 1000 km from the compressive tectonic domain of eastern Anatolia into the broad and diverse tectonic domain of the western Anatol...
Lake Hazar Basin: a Negative Flower Structure on the East Anatolian Fault System (EAFS), SE Turkey
East Anatolian Fault System Lake Hazar basin negative flower structure Turkey
2009/7/7
The East Anatolian Fault System (EAFS) is a 30-km-wide, 700-km-long and NE-trending sinistral strike-slip megashear belt between the Anatolian platelet in the northwest and African-Arabian plates in t...
Quaternary Activity of the Cihanbeyli and Yeniceoba Fault Zones: İnönü-Eskişehir Fault System, Central Anatolia
Neotectonic Quaternary activity kinematic analysis Tuzgö lü Central Anatolia İ nö nü-Eskiş ehir fault system Cihanbeyli fault zone Yeniceoba fault zone
2009/7/7
The İnönü-Eskişehir fault system (İEFS) is one of the most important fault systems in Central Anatolia and consists of a series of NW-SE- to WNW-ESE-trending fault zones extending ...
BARGEN continuous GPS data across the eastern Basin and Range province, and implications for fault system dynamics
satellite geodesy Quaternary normal faulting fault slip continental deformation stress distribution
2014/4/9
We collected data from a transect of continuous GPS sites across the eastern Basin and Range province at latitude 39◦N from 1997–2000. Intersite velocities define a region～350 km wide of broadly...