Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Peter L. Nester"'
Autor:
Karla F. Ojeda, Calogero M. Santoro, Sergio A. Estay, Teresa E. Jordan, Peter L. Nester, Claudio Latorre, Eugenia M. Gayo
Publikováno v:
Earth-Science Reviews. 113:120-140
The hyperarid core of the Atacama Desert possesses important reserves of “fossil” or ancient groundwater, yet the extent and timing of past hydrologic change during the late Quaternary is largely unknown. In situ and/or short-distance transported
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dee1dd3aaf7e46d9e8f31a808ee1db13
https://doi.org/10.1016/j.earscirev.2012.04.003
https://doi.org/10.1016/j.earscirev.2012.04.003
Publikováno v:
Proceedings of the National Academy of Sciences. 104:19724-19729
A large fraction of the vital groundwater in the Atacama Desert of northern Chile is likely composed of “fossil” or “ancient” reserves that receive little or no recharge in today's hyperarid climate. Here, we present evidence for latest Pleis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c5d4d5ea8c41d556be9e8a53e787b6a
https://doi.org/10.1073/pnas.0705373104
https://doi.org/10.1073/pnas.0705373104
Autor:
Warren D. Allmon, James M. Sherpa, Paul G. Harnik, Peter L. Nester, Robert M. Ross, John J. Chiment, Andrew M. Goldman
Publikováno v:
Journal of Geoscience Education. 51:39-47
An important long-term goal of science education reform is to involve more students in open-ended inquiry and authentic research. In making such “research partnerships” between scientists and students commonplace, it is critical to determine how
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f5180945a613bd97fd274232a0eddd0
https://doi.org/10.5408/1089-9995-51.1.39
https://doi.org/10.5408/1089-9995-51.1.39
Publikováno v:
Quaternary Research. 57:225-233
Holocene sediments from Nelson Lake, on Michigan's eastern Upper Peninsula, provide isotopic, pollen, and charcoal evidence for a two-step sequence of changes in moisture source and increased lake-effect precipitation during the late Holocene. Betwee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::adc085f8995cb0e44f8cf46ecf81a756
https://doi.org/10.1006/qres.2001.2308
https://doi.org/10.1006/qres.2001.2308
Autor:
Peter L. Nester, Teresa E. Jordan
Publikováno v:
Tectonics of Sedimentary Basins
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19600bcfd04959ee73aaf09538ce7b5f
https://doi.org/10.1002/9781444347166.ch18
https://doi.org/10.1002/9781444347166.ch18
Autor:
Federico M. Dávila, Gregory D. Hoke, Teresa E. Jordan, Andrew J. Tomlinson, Nicolás Blanco, Peter L. Nester
Publikováno v:
Tectonics. 29
[1] The western flank of the Central Andean Plateau is a crustal-scale monoclinal fold, expressed in the geomorphology and in the westward tilt of fore-arc basin strata. Data from three fore-arc basins quantify the magnitude and time of displacement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4997cbc6ab0ec5d7aa89d422ba615ad
https://doi.org/10.1029/2010tc002661
https://doi.org/10.1029/2010tc002661