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Bala (Ankara) Earthquakes: Implications for Shallow Crustal Deformation in Central Anatolian Section of the Anatolian Platelet (Turkey)
Bala (Ankara) Earthquakes Shallow Crustal Deformation Central Anatolian Section of the Anatolian Platelet
2010/10/14
Central Anatolia is quiet in terms of seismic activity, and rarely earthquakes up to magnitude 5.6 occur in the inner part of the Anatolian block or Anatolian platelet. Southeast of Ankara, the capita...
Detection of millimetric deformation using a terrestrial laser scanner:experiment and application to a rockfall event
millimetric deformation terrestrial laser scanner rockfall event
2009/12/16
Terrestrial laser scanning (TLS) is one of the most promising surveying techniques for rockslope characterization and monitoring. Landslide and rockfall movements can be detected by means of compariso...
Stress induced polarization currents and electromagnetic emission from rocks and ionic crystals, accompanying their deformation
polarization currents electromagnetic emission rocks ionic crystals stress
2009/12/14
A crucial question of the scientific community nowadays, concerns the existence of electric signals preceding earthquakes. In order to give a plausible answer to this question, we carried out two kind...
Distributed power-law seismicity changes and crustal deformation in the SW Hellenic ARC
power-law seismicity changes crustal deformation SW Hellenic ARC
2009/12/11
A region of definite accelerating seismic release rates has been identified at the SW Hellenic Arc and Trench system, of Peloponnesus, and to the south-west of the island of Kythera (Greece). The iden...
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
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...
Detection of millimetric deformation using a terrestrial laser scanner:experiment and application to a rockfall event
millimetric deformation terrestrial laser scanner rockfall event
2009/12/8
Terrestrial laser scanning (TLS) is one of the most promising surveying techniques for rockslope characterization and monitoring. Landslide and rockfall movements can be detected by means of compariso...
Kinematics and timing of polyphase post-Caledonian deformation in the Bergen area,SW Norway
Kinematics timing polyphase post-Caledonian deformation Bergen area
2009/12/3
Polyphase semi-brittle to brittle deformation of the basement rocks of the Øygarden Complex commenced shortly after Caledonian ESE-directed thrusting and followed ductile W-directed shearing. T...
Rock-slope failures in Norway;type,geometry,deformation mechanisms and stability
Rock-slope failures type geometry deformation mechanisms stability
2009/12/3
Extensive studies of Norwegian rock-slope failure areas support a subdivision into three principle types: (1) Rockfall areas, (2) rockslide areas, and (3) complex fields. The classification is based o...
Soft-sediment deformation structures in the Late Silurian Stubdal Formation:the result of seismic triggering
Soft-sediment deformation structures Late Silurian Stubdal Formation seismic triggering
2009/12/3
The Ringerike Group is a lower Old Red Sandstone fluvial sequence that forms part of the Late Silurian foreland basin succession of the Ringerike Group, Oslo Region, southern Norway. The Ringerike Gro...
Age constraints on the late Caledonian (Scandian) deformation in the Major Bergen Arc,SW Norway
Age constraints late Caledonian deformation Major Bergen Arc
2009/12/3
The Ulven Syncline in the Bergen Arcs contains some of the youngest rocks involved in Caledonian orogenic deformation in West Norway. The pelitic Vaktdal Formation contains a Middle Llandovery (439-43...
Inhomogeneous deformation in deeply buried continental crust,an example from the eclogite-facies province of the Western Gneiss Region,Norway
Inhomogeneous deformation continental crust eclogite-facies province Western Gneiss Region
2009/12/2
Mesoproterozoic protoliths and Scandian eclogites with coronitic textures were preserved in low-strain domains during burial and exhumation in the Sunnfjord Region of western Norway. In domains with m...
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
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...
Ground deformation detection of the greater area of Thessaloniki (Northern Greece) using radar interferometry techniques
Ground deformation detection the greater area radar interferometry techniques
2009/12/30
In the present study SAR interferometric techniques (stacking of conventional interferograms and Permanent Scatterers), using images from satellites ERS-1 and 2, have been applied to the region of The...
Using Bayesian methods for the parameter estimation of deformation monitoring networks
Bayesian methods the parameter estimation deformation monitoring networks
2009/12/30
In order to investigate the deformations of an area or an object, geodetic observations are repeated at different time epochs and then these observations of each period are adjusted independently. Fro...
专著信息
书名
Cenozoic deformation of the Tarim basin and its implications for collisional mountain building in Tibetan plateau and Tian Shan
语种
英文
撰写或编译
作者
Yang Y.,Liu M.
第一作者单位
出版社
v. 21, p. 1059, doi:10...