Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Brian G. Hough"'
Autor:
Brian G. Hough, Weitao Wang, Ying Wu, Li Yang, Dewen Zheng, Jing Yang, Hua-Ning Qiu, Wen Chen
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 445:83-96
40Ar/39Ar incremental-heating analyses of supergene jarosite and yavapaiite were conducted for three weathering profiles at the Hongshan, Liuhuangshan, and Caihuagou deposits in the Tu–Ha Basin. The analyses provide numerical constraints on the tim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e5cc95c2dc108edc1ea192c2d63b5d0
https://doi.org/10.1016/j.palaeo.2016.01.005
https://doi.org/10.1016/j.palaeo.2016.01.005
Publikováno v:
Earth and Planetary Science Letters. 408:35-47
The timing and mechanism of the formation of the high elevations of the central Rocky Mountains (Rockies) in the western interior of North America remain controversial. We examine the middle and late Cenozoic paleorelief between the Great Plains and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91115895318f84af05e8d8e0b0c9c449
https://doi.org/10.1016/j.epsl.2014.09.050
https://doi.org/10.1016/j.epsl.2014.09.050
Publikováno v:
Geology. 42:547-550
When and how the central Rocky Mountains (Rockies) of western North America gained modern topography remain controversial questions. We reconstruct the middle and late Cenozoic topography along a transect that extends from the Great Plains of western
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8782225b8a968be577bf4f4f8f57f5b7
https://doi.org/10.1130/g35444.1
https://doi.org/10.1130/g35444.1
Publikováno v:
Earth and Planetary Science Letters. 391:110-120
Recent work has shown that soil carbonates typically form as the soil dries after seasonal rainfall, and therefore record seasonal aspects of climate rather than mean annual conditions. Because soil carbonate formation is closely related to the timin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94673817f7a415a3984e19fc40254f01
https://doi.org/10.1016/j.epsl.2014.01.008
https://doi.org/10.1016/j.epsl.2014.01.008
Autor:
Jianhui Liu, Daoyang Yuan, Carmala N. Garzione, Dewen Zheng, Chuanyou Li, Guang-Liang Zhang, Richard O. Lease, Zhicai Wang, Brian G. Hough, Peizhen Zhang, Qinglong Wu
Publikováno v:
Journal of Asian Earth Sciences. 44:189-202
Based on field mapping, section measurement and magnetostratigraphy, ∼1700 m of sedimentary rocks have accumulated in the Wushan basin between ∼16 Ma and ∼6 Ma. Basin geometry, sedimentation characteristics and the early syn-depositional deform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3d52f7d8496a61d7088b4acbf3f95a0
https://doi.org/10.1016/j.jseaes.2011.06.009
https://doi.org/10.1016/j.jseaes.2011.06.009
Autor:
Carmala N. Garzione, Richard O. Lease, Douglas W. Burbank, Zhicai Wang, Brian G. Hough, Daoyang Yuan
Publikováno v:
Geological Society of America Bulletin. 123:168-185
Lithologic, magnetostratigraphic, and stable isotope records from the Neogene Xunhua and Linxia basins along the Tibetan Plateau9s northeastern margin suggest that topography in the intervening Jishi Shan mountain range began to develop between 16 an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b9e95d367124416a248597dd92e871e
https://doi.org/10.1130/b30090.1
https://doi.org/10.1130/b30090.1
Autor:
Wen Jun Zheng, Wei Peng Ge, Daoyang Yuan, Eric Kirby, Katherine E. Dayem, Peter Molnar, Peizhen Zhang, William H. Craddock, Zhi Cai Wang, Richard O. Lease, Gerard H. Roe, Douglas W. Burbank, Jean-Daniel Champagnac, Huiping Zhang, Brian G. Hough, Marin K. Clark, Carmala N. Garzione, Chuanyou Li, Dewen Zheng, Zhen Wei Chen, Kenneth A. Farley, Alison R. Duvall
Publikováno v:
Tectonics, vol 32, iss 5
Tectonics
Yuan, DY; Ge, WP; Chen, ZW; Li, CY; Wang, ZC; Zhang, HP; et al.(2013). The growth of northeastern Tibet and its relevance to large-scale continental geodynamics: A review of recent studies. Tectonics, 32(5), 1358-1370. doi: 10.1002/tect.20081. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/24g0x670
Tectonics
Yuan, DY; Ge, WP; Chen, ZW; Li, CY; Wang, ZC; Zhang, HP; et al.(2013). The growth of northeastern Tibet and its relevance to large-scale continental geodynamics: A review of recent studies. Tectonics, 32(5), 1358-1370. doi: 10.1002/tect.20081. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/24g0x670
Recent studies of the northeastern part of the Tibetan Plateau have called attention to two emerging views of how the Tibetan Plateau has grown. First, deformation in northern Tibet began essentially at the time of collision with India, not 10-20 Myr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd1e3f5b2567759fbafc02fbe09eeef1
https://resolver.caltech.edu/CaltechAUTHORS:20131220-155301622
https://resolver.caltech.edu/CaltechAUTHORS:20131220-155301622
Publikováno v:
Geological Society of America Bulletin, vol 124, iss 5-6
Lease, RO; Burbank, DW; Hough, B; Wang, Z; & Yuan, D. (2012). Pulsed Miocene range growth in northeastern Tibet: Insights from Xunhua Basin magnetostratigraphy and provenance. Bulletin of the Geological Society of America, 124(5-6), 657-677. doi: 10.1130/B30524.1. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/6n73c02p
Bulletin of the Geological Society of America, vol 124, iss 5-6
Lease, RO; Burbank, DW; Hough, B; Wang, Z; & Yuan, D. (2012). Pulsed Miocene range growth in northeastern Tibet: Insights from Xunhua Basin magnetostratigraphy and provenance. Bulletin of the Geological Society of America, 124(5-6), 657-677. doi: 10.1130/B30524.1. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/6n73c02p
Bulletin of the Geological Society of America, vol 124, iss 5-6
Author(s): Lease, RO; Burbank, DW; Hough, B; Wang, Z; Yuan, D | Abstract: Sedimentary rocks in Tibetan Plateau basins archive the spatiotemporal patterns of deformation, erosion, and associated climate change that resulted from Cenozoic continental c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2aa3acd580143d1182b1c29dfa0c73e6
https://escholarship.org/uc/item/6n73c02p
https://escholarship.org/uc/item/6n73c02p