a great earthquake in history(passive) caused bycrustal deformation
earthquake - related and volcanic processescausecrustal deformation
the 2011 off the Pacific coast of Tohoku Earthquake(passive) caused bycrustal deformation
Fault movement ( earthquake ) under the seafloorcausescrustal deformation
the 2016 Kumamoto earthquake revealed by GEONET / Satoshi Kawamoto in Bulletin of the GeoSpatial Information authority of Japan(passive) caused byCrustal deformation
the Nepal ( Gorkha ) Earthquake Using ALOS-2 SAR Interferometry(passive) Caused byCrustal Deformation
magma migration in the northern Izu Islands , Japan , Geophys(passive) caused byCrustal deformation
glacioisostatic uplift , which is going on until now(passive) caused bycrustal deformation
the tectonics activities(passive) caused byCrustal deformation
the 2016 Kumamoto Earthquake Revealed by GEONET Satoshi KAWAMOTO , Yohei HIYAMA , Reiko KAI , Fumio SUGA , Kazunori YAMAGUCHI , Tomoaki FURUYA , Satoshi ABE and Naofumi TAKAMATSU GNSS observation over the area of the 2016 Kumamoto Earthquake(passive) Caused by・Crustal Deformation
seasonal filling and emptying of four surface reservoirs of varying dimensions located in different geological domains of India(passive) caused bycrustal deformation
subsidence ( a decrease in the ground ’s elevation ) , landslides , earthquakes and volcanic activity(passive) caused bycrustal deformation
megathrust faulting ( Kato et al . 2011(passive) caused bycrustal deformation
an eruption of Mount Shinmoe(passive) caused byCrustal deformation
magmatic and tectonic processes(passive) caused bycrustal deformation
This interseismic stress relaxationcausescrustal deformation
Orogenesiscausescrustal deformation
three mechanismscausingcrustal deformation
hot spots and volcanic lava(passive) caused bycrustal deformation
time - varying TWS(passive) caused bycrustal deformation
extension in the western USA , Nature , 464 , Number 7290(passive) caused bywidespread crustal deformation
subduction of the underlying mantle(passive) caused bycrustal deformation
the rifting and spreading of the Okinawa Trough , which is viewed as a continuation of the Beppu – Shimabara graben ( Tada 1985(passive) caused bycrustal deformation
the intrusion of a magma body into the shallow depth region(passive) caused bycrustal deformation
the earthquakes along the fault(passive) caused bycrustal deformation
from glaco build - up and decay of great ice sheetsresultingfrom glaco build - up and decay of great ice sheets
to a positive feedback between erosion at the surface and shortening of the crust[Avouac and Burov , 1996]leadingto a positive feedback between erosion at the surface and shortening of the crust[Avouac and Burov , 1996]
gravity change(passive) are caused bygravity change
from the subduction of the Juan de Fuca oceanic plate beneath the North American continentresultingfrom the subduction of the Juan de Fuca oceanic plate beneath the North American continent
fluid migration(passive) caused byfluid migration
separation along a boundary of rock types ... typically between so - called crystalline " basement " rock and overlying sedimentary rockscausesseparation along a boundary of rock types ... typically between so - called crystalline " basement " rock and overlying sedimentary rocks
cracks that are much better conductors than solid rockcreatescracks that are much better conductors than solid rock
a Fault - a major cross - formation break with accompanying displacement o … f one side against the other(passive) caused tectonically bya Fault - a major cross - formation break with accompanying displacement o … f one side against the other
a glaciation cyclecausesa glaciation cycle
in increased crustal thickness and possibly dehydration and/or melting of thickened lower continental crustresultingin increased crustal thickness and possibly dehydration and/or melting of thickened lower continental crust
Horizontal and vertical offset(passive) caused byHorizontal and vertical offset
Subsidence , which refers to “ the loss of surface elevation due to removal of subsurface support , ” ... sediment compaction ; withdrawal of groundwater , hydrocarbons , geothermal fluids or minerals ( sulphur ) ; and dewatering of organic soils(passive) is caused bySubsidence , which refers to “ the loss of surface elevation due to removal of subsurface support , ” ... sediment compaction ; withdrawal of groundwater , hydrocarbons , geothermal fluids or minerals ( sulphur ) ; and dewatering of organic soils
several geophysical phenomenacausesseveral geophysical phenomena
to fracturesleadsto fractures
faulting(passive) caused byfaulting
from ALOS-2 / PALSAR-2 datacreatedfrom ALOS-2 / PALSAR-2 data
from the ongoing extensionalresultingfrom the ongoing extensional
gravity anomaliescausesgravity anomalies
from natural hazards at hourly intervalsresultingfrom natural hazards at hourly intervals
zones of weakness within the cratonic ( basement ) layer which in turn produced channels through which magma could move , thereby forming intrusive and extrusive rockscreatedzones of weakness within the cratonic ( basement ) layer which in turn produced channels through which magma could move , thereby forming intrusive and extrusive rocks
in both faults and foldsresultsin both faults and folds
to the preservation of subsided marshesmay also contributeto the preservation of subsided marshes
from instantaneous events ( e.g. earthquakesresultingfrom instantaneous events ( e.g. earthquakes
from earthquakes and volcanoesresultingfrom earthquakes and volcanoes
to great - earthquakes in Sumatra over the last 7,000 yearsleadingto great - earthquakes in Sumatra over the last 7,000 years
the surface of the Earth to change constantlycausesthe surface of the Earth to change constantly
to tectonic consequencesleadingto tectonic consequences
from convergence of the two tectonic platesresultingfrom convergence of the two tectonic plates
to geochemical variation in emitted gasesledto geochemical variation in emitted gases
to the stratigraphycontributingto the stratigraphy
gravity changes(passive) caused bygravity changes
volcanic eruption or near field earthquake action such as reservoircould triggervolcanic eruption or near field earthquake action such as reservoir
shallower earthquakes at a great distance from the trench(passive) to be caused byshallower earthquakes at a great distance from the trench