very slowlycausingvery slowly

the long - posited idea(passive) should be influenced bythe long - posited idea

surface exhumationinfluencedsurface exhumation

west of the backarcoriginatingwest of the backarc

this surface unroofing because the model predicts Late Jurassic dynamic uplift , Cretaceous dynamic subsidence , early Cenozoic dynamic uplift and late Cenozoic dynamic subsidenceinfluencedthis surface unroofing because the model predicts Late Jurassic dynamic uplift , Cretaceous dynamic subsidence , early Cenozoic dynamic uplift and late Cenozoic dynamic subsidence

basin , which is constructing under N - S extension field with right - lateral , and continental pull apart(passive) is influenced bybasin , which is constructing under N - S extension field with right - lateral , and continental pull apart

the initial breakup of the supercontinenttriggeredthe initial breakup of the supercontinent

a model of plate velocities(passive) triggered bya model of plate velocities

to the subduction of the Indian Plate as far as the BNS and the transition from the asthenospheric layer to the metasomatic lid overlaps with the transition from north – south shortening in south Tibet to eastward tectonic escape in north Tibet ( Qiangtang and Songpan – Ganzi blockscontributesto the subduction of the Indian Plate as far as the BNS and the transition from the asthenospheric layer to the metasomatic lid overlaps with the transition from north – south shortening in south Tibet to eastward tectonic escape in north Tibet ( Qiangtang and Songpan – Ganzi blocks

dynamic topography(passive) is being created bydynamic topography

howevercan ... resulthowever

Hawaii - Emperor Seamount(passive) caused byHawaii - Emperor Seamount

elevation differences(passive) caused byelevation differences

observed planetary topography - crustal isostasy , elastic support and dynamic support(passive) caused byobserved planetary topography - crustal isostasy , elastic support and dynamic support

in on a planet such as Venus with high surface temperatures and a weak lithospheresetin on a planet such as Venus with high surface temperatures and a weak lithosphere

to the Indian plate subduction as far as the BNScontributesto the Indian plate subduction as far as the BNS

plate motionscausesplate motions

to the long - wavelength subsidence of the Siwalik foreland basincontributesto the long - wavelength subsidence of the Siwalik foreland basin

The strain deformations(passive) caused byThe strain deformations

The transition to anisotropy(passive) caused byThe transition to anisotropy

plate motionis leadingplate motion

continents(passive) caused bycontinents

Quakes away from plate boundaries(passive) may be triggered byQuakes away from plate boundaries

significantly to present - day polar wandercontributessignificantly to present - day polar wander

changes in melt production and composition at volcanic arcscan causechanges in melt production and composition at volcanic arcs

the lithosphere under compression in mainland China ... and is a possible main cause of the lithospheric stress in Alashan , Qaidam , western Tibetan and eastern Tarim blocks as well as the east of the eastern Chinacausesthe lithosphere under compression in mainland China ... and is a possible main cause of the lithospheric stress in Alashan , Qaidam , western Tibetan and eastern Tarim blocks as well as the east of the eastern China

deformation(passive) caused bydeformation

normal stress and tangential stressescausesnormal stress and tangential stresses

from downdip slab motionresultingfrom downdip slab motion