Zobrazeno 1 - 10
of 16
pro vyhledávání: '"James V. Hengesh"'
Publikováno v:
GSA Bulletin. 134:1614-1620
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::edaab6778ccdbc121f352e8e8d4c8c81
https://doi.org/10.1130/b36135.1
https://doi.org/10.1130/b36135.1
Publikováno v:
Tectonophysics. 686:1-18
We have investigated the locations and patterns of neotectonic deformation in the Carnarvon basin along the Mesozoic rifted margin of Western Australia to evaluate the characteristics of post-Neogene tectonic reactivation. Geological, geophysical, ge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd9a1b25deff818518f50cbe3cc4633e
https://doi.org/10.1016/j.tecto.2016.06.008
https://doi.org/10.1016/j.tecto.2016.06.008
Autor:
James V. Hengesh, Beau B. Whitney
Publikováno v:
Tectonics. 35:1066-1089
Australia's northwestern passive margin intersects the eastern termination of the Java trench segment of the Sunda arc subduction zone and the western termination of Timor trough along the Banda arc tectonic collision zone. Differential relative moti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56f913c43c9a0f6866496291c2620d64
https://doi.org/10.1002/2015tc004103
https://doi.org/10.1002/2015tc004103
Publikováno v:
Geological Society of America Bulletin. 128:684-704
Our paleoseismological study of faults and fault-related folds comprising the Mount Narryer fault zone reveals a mid- to late Quaternary history of repeated morphogenic earthquakes that have influenced the planform and course of the Murchison, Roderi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49c1c529deed4a9e688064f7d7434e11
https://doi.org/10.1130/b31313.1
https://doi.org/10.1130/b31313.1
Autor:
Beau B. Whitney, James V. Hengesh
Publikováno v:
Geomorphology. 241:160-174
A late Pleistocene (Marine Isotope Stage 5e) emergent marine sequence fringes the coastline of the Cape Region of coastal west central Australia and provides elevation and age control to characterize the locations and rates of crustal deformation. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fcf044dd74536cd7493317d1309f675c
Autor:
James V. Hengesh, Beau B. Whitney
Publikováno v:
Geomorphology. 228:579-596
This study examines channel-scale morphodynamics of ephemeral streams in the onshore Carnarvon basin in arid west-central Western Australia. The rivers in this region have low gradients, the landscape has low relief, and the rates of climatically and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::59cd4738d9feb4e3ee7f62359b6a6520
https://doi.org/10.1016/j.geomorph.2014.10.020
https://doi.org/10.1016/j.geomorph.2014.10.020
Autor:
David Baumont, James V. Hengesh
Publikováno v:
Encyclopedia of Maritime and Offshore Engineering
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3437773a26dbeb35fb2e651de7366f1d
https://doi.org/10.1002/9781118476406.emoe520
https://doi.org/10.1002/9781118476406.emoe520
Publikováno v:
Australian Journal of Earth Sciences. 59:341-354
A temporary seismic network deployed in northwestern Australia between October 2005 and March 2008 recorded 28 earthquakes ranging in magnitude between M L 2.0 and M L 5.3. Twenty-three of these events occurred in areas underlain by continental crust
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d1aad698bda8e3bbf227f9ef5bcc684
https://doi.org/10.1080/08120099.2012.667439
https://doi.org/10.1080/08120099.2012.667439
Publikováno v:
Quarterly Journal of Engineering Geology and Hydrogeology. 42:251-259
The Camisea pipeline system, Peru, comprises two buried pipelines within the same right-of-way; a natural gas line (714 km) and a natural gas liquids (NGL) line (540 km). The pipelines originate at the Camisea gas field near Malvinas in the Amazon ju
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a053f76f69d6a940f3d44cbce734111
https://doi.org/10.1144/1470-9236/08-061
https://doi.org/10.1144/1470-9236/08-061
Publikováno v:
Tectonophysics. 392:279-301
Many bends or step-overs along strike–slip faults may evolve by propagation of the strike–slip fault on one side of the structure and progressive shut-off of the strike–slip fault on the other side. In such a process, new transverse structures
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eaf95c25b3ad8ee8f2f4fbbb1a8497b0
https://doi.org/10.1016/j.tecto.2004.04.013
https://doi.org/10.1016/j.tecto.2004.04.013