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A note on the boundary contribution with bad deformation in gauge theory
BCFW recursion relation gauge field theory boundary contribution
2018/4/19
Motivated by recently progresses in the study of BCFW recursion relation with nonzero bound-ary contributions for theories with scalars and fermions[1], in this short note we continue the study of bou...
Development of crystallographic preferred orientation and microstructure during plastic deformation of natural coarse-grained quartz veins
Development of crystallographic preferred orientation and microstructure plastic deformation natural coarse-grained quartz veins
2014/5/20
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 samples of natural monomineralic tabular veins. The veins opened and were= deformed, up to shear str...
An elastic plate model for interseismic deformation in subduction zones
An elastic plate model interseismic deformation in subduction zones
2014/4/9
Geodetic observations of interseismic surface deformation in the vicinity of subduction zones are frequently interpreted using simple kinematic elastic dislocation models (EDM). In this theoretical st...
Deformation inequivalent complex conjugated complex structures and applications
Real structure deformation moduli
2010/3/1
We start from a short summary of our principal result from [KK]: an example of a complex algebraic surface which is not deformation equivalent to its complex conjugate and which, moreover, has no home...
Emergent Noncommutative gravity from a consistent deformation of gauge theory
gravity gauge theory
2010/3/22
Starting from a standard noncommutative gauge theory and using the Seiberg-Witten map we propose a new version of a noncommutative gravity. We use consistent deformation theory starting from a free ga...
Deformation of contour and Hawking temperature
black hole Hawking temperature integral contour
2010/3/18
It was found that, in an isotropic coordinate system, the tunneling approach brings a factor of 1/2 for the Hawking temperature of a Schwarzschild black hole. In this paper, we address this kind of pr...
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...