Space geodesy: A revolution in crustal deformation measurements of tectonic processes

Author(s):  
Roland Bürgmann ◽  
Wayne Thatcher
2018 ◽  
Vol 45 (14) ◽  
pp. 6869-6877 ◽  
Author(s):  
Keiichi Tadokoro ◽  
Mamoru Nakamura ◽  
Masataka Ando ◽  
Hiroshi Kimura ◽  
Tsuyoshi Watanabe ◽  
...  

Author(s):  
Kristine M. Larson ◽  
A. R. Lowry ◽  
Vladimir Kostoglodov ◽  
Wallis Hutton ◽  
Osvaldo Sánchez ◽  
...  

Author(s):  
C. Vita-Finzi

The analysis of crustal deformation by tectonic processes has gained much from the clues offered by drainage geometry and river behaviour, while the interpretation of channel patterns and sequences benefits from information on Earth movements before or during their development. The interplay between the two strands operates at many scales: themes which have already benefited from it include the possible role of mantle plumes in the breakup of Gondwana, the Cenozoic development of drainage systems in Africa and Australia, Himalayan uplift in response to erosion, alternating episodes of uplift and subsidence in the Mississippi delta, buckling of the Indian lithospheric plate, and changes in stream pattern and sinuosity along individual alluvial channels subject to localized deformation. Developments in remote sensing, isotopic dating and numerical modelling are starting to yield quantitative analyses of such effects, to the benefit of geodymamics as well as fluvial hydrology.


2021 ◽  
Vol 8 (1) ◽  
Author(s):  
K. A. McKenzie ◽  
K. P. Furlong

AbstractSeveral tectonic processes combine to produce the crustal deformation observed across the Cascadia margin: (1) Cascadia subduction, (2) the northward propagation of the Mendocino Triple Junction (MTJ), (3) the translation of the Sierra Nevada–Great Valley (SNGV) block along the Eastern California Shear Zone–Walker Lane and, (3) extension in the northwestern Basin and Range, east of the Cascade Arc. The superposition of deformation associated with these processes produces the present-day GPS velocity field. North of ~ 45° N observed crustal displacements are consistent with inter-seismic subduction coupling. South of ~ 45° N, NNW-directed crustal shortening produced by the Mendocino crustal conveyor (MCC) and deformation associated with SNGV-block motion overprint the NE-directed Cascadia subduction coupling signal. Embedded in this overall pattern of crustal deformation is the rigid translation of the Klamath terrane, bounded on its north and west by localized zones of deformation. Since the MCC and SNGV processes migrate northward, their impact on the crustal deformation in southern Cascadia is a relatively recent phenomenon, since ~ 2 –3 Ma.


2002 ◽  
Vol 54 (9) ◽  
pp. 871-881 ◽  
Author(s):  
Takuji Yamada ◽  
Masataka Ando ◽  
Keiichi Tadokoro ◽  
Kazutoshi Sato ◽  
Takashi Okuda ◽  
...  

2018 ◽  
Vol 53 (3) ◽  
pp. 331-345 ◽  
Author(s):  
Eszter Szűcs ◽  
István Bozsó ◽  
István János Kovács ◽  
László Bányai ◽  
Ágnes Gál ◽  
...  

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