Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Amalia C. Doebbert"'
Autor:
David M. Lovelace, Amalia C. Doebbert
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 424:1-5
The Alcova Limestone is a widely exposed but poorly studied Triassic unit found throughout Wyoming. Although it is used as a regional lithostratigraphic marker bed, the age of the limestone is not well constrained and contention regarding its deposit
Autor:
Meredith Rhodes Carson, Alan R. Carroll, Jeffrey T. Pietras, Brian L. Beard, Amalia C. Doebbert, Brooke Ann Norsted, Clark M. Johnson, L. Ashley Throckmorton
Publikováno v:
Chemical Geology. 380:172-189
Strontium isotopes from lacustrine carbonates record detailed weathering histories of exposed bedrocks, and thus are potentially useful for understanding interactions between tectonics and climate that may be driven by local or regional factors in ba
Publikováno v:
Journal of Sedimentary Research. 82:841-858
Detrital zircon U/Pb ages and Pb isotope compositions of detrital feldspars from the Late Cretaceous–Eocene Gualala Basin in northern California indicate that the basin received sediments from the southern Sierra Nevada, the Mojave block, and the S
Publikováno v:
Geological Society of America Bulletin. 122:236-252
Oxygen isotope values from lacustrine carbonate in the Laney Member of the Green River Formation (Wyoming) exhibit a sudden, basinwide, ~6‰ upsection decrease in δ 18 O at ca. 49 Ma. 40 Ar/ 39 Ar geochronology constrains the duration of the isotop
Autor:
Malinda Louise Kent-Corson, Zhou Wang, Bradley B. Sageman, Peter M. Blisniuk, C. Page Chamberlain, Stephan A. Graham, Wang Chengshan, Xiaoqiao Wan, Amalia C. Doebbert, Alan R. Carroll
Because of the need to understand the links and feedbacks of the carbon cycle during times of global greenhouse conditions numerous studies have focused on the Cretaceous climate. Much of what we know about this warm period in Earth's history comes f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d7f7f8b95ad8344044d72f33a2be075d
https://hdl.handle.net/10356/105847
https://hdl.handle.net/10356/105847
Autor:
Clark M. Johnson, C. Page Chamberlain, M. Elliot Smith, Brian L. Beard, Meredith K. Rhodes-Carson, Amanda L. Booth, Amalia C. Doebbert, Alan R. Carroll
Publikováno v:
Geology. 36:791
Sedimentary facies of the Eocene Green River Formation refl ect a rapid increase in water supply to Lake Gosiute ca. 49 Ma, marked by a stratigraphic fi ll-to-spill surface. Deposits below this surface constitute repetitive lacustrine expansion-desic