搜索结果: 1-15 共查到“理学 North Anatolian Fault”相关记录16条 . 查询时间(0.12 秒)
Crustal structure at the western end of the North Anatolian Fault Zone from deep seismic sounding
north Anatolian fault zone crustal structure deep seismic sounding
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2015/9/28
The first deep seismic sounding experiment in Northwestern Anatolia was carried out in October 1991 as part of the "German - Turkish Project on Earthquake Prediction Research" in the Mudurnu area of t...
A 3000-year record of surface-rupturing earthquakes at Günalan: variable fault-rupture lengths along the 1939 Erzincan earthquake-rupture segment of the North Anatolian Fault, Turk
paleoseismology North Anatolian Fault fault segment
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2015/8/26
The North Anatolian Fault is a ca. 1200-km-long, right-lateral, strike-slip fault that forms the northern boundary of the Anatolian plate. A damaging sequence of earthquakes ruptured almost the entire...
Paleoseismic record obtained by coring a sag-pond along the North Anatolian Fault (Turkey)
Paleoseismology seismites sedimentary cores North Anatolian Fault
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2015/8/26
Shallow lakes along minor structural bends or discontinuities of strike-slip faults are not usually paleoseismological target sites. In the present study, we show that a 2-m-deep, 700-m-long lake that...
Submarine Paleoseismology Along Populated Transform Boundaries: The Enriquillo-Plantain-Garden Fault, Canal du Sud, Haiti, and the North Anatolian Fault, Marmara Sea, Turkey
Populated Transform Boundaries Submarine Paleoseismology
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2015/7/17
Continental transform boundaries cross heavily populated regions and are associated with destructive earthquakes worldwide. The devastating 1999 Turkey earthquakes and the offshore 2010 Haiti earthqua...
Faulting and Stress Distribution in the Bolu Pull-apart Basin (North Anatolian Fault Zone, Turkey): The Significance of NewDates Obtained from the Basin Fill
features earth siences earthquakes
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2011/3/22
The Bolu Basin in northwestern Turkey, situated in the western part of the North Anatolian Fault Zone (NAFZ), displays the neotectonic features of a pull apart basin. The long axis of the basin exten...
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
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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. ...
Investigation of long period crustal deformation on the inactive branch of the North Anatolian Fault Zone
long period crustal deformation inactive branch North Anatolian Fault Zone
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2009/12/8
The western part of North Anatolian Fault (NAF) bifurcates around Mudurnu into two fault segments: northern and southern branch. The latter bifurcates again at west of Pamukova and creates middle stra...
Temporal variations of the fractal properties of seismicity in the western part of the north Anatolian fault zone:possible artifacts due to improvements in station coverage
Temporal variations fractal properties of seismicity north Anatolian fault zone
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2009/11/16
Seismically-active fault zones are complex natural systems exhibiting scale-invariant or fractal correlation between earthquakes in space and time, and a power-law scaling of fault length or earthquak...
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
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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
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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
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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...
The Relationship Between the Tectonic Setting of the Lake İznik Basin and the Middle Strand of the North Anatolian Fault
North Anatolian Fault Lake İ znik tectonics high-resolution seismic data releasing bend
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2009/7/7
The İznik Basin is an active depression created by a series of faults developed in relation to the Middle Strand of the North Anatolian Fault (NAFMS). The most important of these faults is the ob...
Investigation of long period crustal deformation on the inactive branch of the North Anatolian Fault Zone
long period crustal deformation inactive branch North Anatolian Fault Zone
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2009/12/16
The western part of North Anatolian Fault (NAF) bifurcates around Mudurnu into two fault segments: northern and southern branch. The latter bifurcates again at west of Pamukova and creates middle stra...
Triggered creep rate on the Ismetpasa segment of the North Anatolian Fault
creep rate Ismetpasa segment North Anatolian Fault
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2010/1/4
The Ismetpasa segment of the North Anatolian Fault is one of the rare places in the world where aseismic creep event has been observed. This segment was ruptured during both the 1944, Mw=7.2, Gerede a...
The Relationship Between the Tectonic Setting of the Lake İznik Basin and the Middle Strand of the North Anatolian Fault
North Anatolian Fault Lake İ znik tectonics high-resolution seismic data releasing bend
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2010/1/11
The İznik Basin is an active depression created by a series of faults developed in relation to the Middle Strand of the North Anatolian Fault (NAFMS). The most important of these faults is the ob...