Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Whitney J. Autin"'
Autor:
Joann Mossa, Whitney J. Autin
Publikováno v:
Aggregate Resources ISBN: 9781003077954
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9eade7854e46bcb226047d68acb7ae91
https://doi.org/10.1201/9781003077954-28
https://doi.org/10.1201/9781003077954-28
Autor:
Whitney J. Autin
Publikováno v:
The Anthropocene Review. 3:218-230
Anthropocene has developed a varied set of connotations among scientific and non-scientific advocates. As a result, multiple dichotomies of the Anthropocene exist within various scholarly disciplines. The Anthropocene allows people to reinforce and p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81d8a423e038d5d9d7eb9777b1832386
https://doi.org/10.1177/2053019616646133
https://doi.org/10.1177/2053019616646133
Autor:
Whitney J. Autin, Marc J. P. Gouw
Publikováno v:
Sedimentary Geology. 204:106-121
The proportion and arrangement of channel-belt deposits in alluvial successions (alluvial architecture) is not known in detail for most modern settings. Therefore, the alluvial architecture of the Holocene Lower Mississippi Valley (LMV) between Green
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43868df1cf29b5565b874dea07db7ee7
https://doi.org/10.1016/j.sedgeo.2008.01.003
https://doi.org/10.1016/j.sedgeo.2008.01.003
Publikováno v:
Tectonophysics. 420:431-454
The earthquake cycles that characterize continental-interior areas that are far from active plate boundaries have proven highly cryptic and difficult to resolve. We used a novel paleoseismic proxy to address this issue. Namely, we reconstructed Holoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f9b9fd3cdc38ce74f09dfcf6bc99a5c
https://doi.org/10.1016/j.tecto.2006.04.002
https://doi.org/10.1016/j.tecto.2006.04.002
Publikováno v:
Journal of Sedimentary Research. 75:650-664
The emphasis on gradient advantages in studies of avulsion is misleading. While gradient advantages are necessary for an avulsion to occur, the late Holocene avulsion history of the Mississippi River in Louisiana suggests that factors such as substra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8dfa9298cc2f9d8031c9e14896cb43c7
https://doi.org/10.2110/jsr.2005.053
https://doi.org/10.2110/jsr.2005.053
Autor:
Whitney J. Autin
Publikováno v:
Geomorphology. 47:227-244
The Five Islands of south central Louisiana are piercement-type salt domes uplifted from several kilometers depth as the surrounding strata experiences regional subsidence. In general, the domes are nearly circular in plan with maximum land surface e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::404be295eafc67eb2a4b787a10701cd7
https://doi.org/10.1016/s0169-555x(02)00086-7
https://doi.org/10.1016/s0169-555x(02)00086-7
Autor:
Andres Aslan, Whitney J. Autin
Publikováno v:
Geological Society of America Bulletin. 113:1456-1466
Comparison of Pleistocene and Holocene soils developed in Mississippi River meander-belt deposits in Louisiana illustrates the influence of relative sea-level change on pedogenesis. Holocene and Pleistocene meander belts have similar landscape morpho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::59d1fae546a6bd50b7bc837b63a92f8d
https://doi.org/10.1130/0016-7606(2001)113<1456:apipah>2.0.co
https://doi.org/10.1130/0016-7606(2001)113<1456:apipah>2.0.co
Autor:
Andres Aslan, Whitney J. Autin
Publikováno v:
Journal of Sedimentary Research. 69:800-815
The alluvial architecture and soil characteristics of Holo cene Mississippi River floodplain deposits in the southern Lower Mississippi Valley provide evidence for significant changes in floodplain development in response to sea-level rise. Floodplai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f688c2c1405cbf2edde46abef900942
https://doi.org/10.2110/jsr.69.800
https://doi.org/10.2110/jsr.69.800