Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Juan A. Vázquez-Navarro"'
Autor:
David Domínguez-Villar, Sonja Lojen, Juan A. Vázquez-Navarro, José Antonio López-Sáez, Kristina Krklec, Miriam Dorado-Valiño, Ian J. Fairchild
Publikováno v:
Scientific Reports, Vol 10, Iss 1, Pp 1-10 (2020)
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scientific Reports
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scientific Reports
The controls that affect the structure and timing of terminations are still poorly understood. We studied a tufa deposit from the Iberian Peninsula that covers Termination II (T-II) and whose chronology was synchronized to speleothem records. We used
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::37b2b0509f8931cdf36b48153f381290
https://doi.org/10.1038/s41598-020-72121-4
https://doi.org/10.1038/s41598-020-72121-4
Publikováno v:
Earth Surface Processes and Landforms. 42:245-258
The precipitation of freshwater carbonates (tufa) along karstic rivers is enhanced by degassing of carbon dioxide (CO2) downstream of karstic springs. However, in most karstic springs CO2 degassing is not enough to force the precipitation of tufa sed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af1255627e0d0f2e77ada5f10b5cc847
https://doi.org/10.1002/esp.3978
https://doi.org/10.1002/esp.3978
Autor:
Ian J. Fairchild, Sonja Lojen, Kristina Krklec, David Domínguez-Villar, Juan A. Vázquez-Navarro
Tufa sediments are freshwater carbonates that precipitate in karst regions after degassing of CO2 from groundwater in contact with the atmosphere. When laminated, these carbonates can provide high-resolution records for the study of climate, hydrolog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2d67366bad482f7d7b134efcdca4caac
https://doi.org/10.1111/sed.12350
https://doi.org/10.1111/sed.12350
Publikováno v:
Geomorphology. :15-25
During the Holocene a series of tufa sediments were deposited from a karstic spring along the Trabaque Canyon, central Spain. A long-term lowering of the water table caused the location of the spring to be displaced from the upper sector of the canyo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1442051946d581e897cfb94c9f3a0d7a
https://doi.org/10.1016/j.geomorph.2012.03.028
https://doi.org/10.1016/j.geomorph.2012.03.028
Publikováno v:
Global and Planetary Change. 77:129-141
The sedimentation of spring-fed tufa deposits is subject to two main factors: the ground water discharge from the spring and the supersaturation of such waters with respect to carbonate at the surface. In Trabaque Canyon (central Spain), several spri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f22737f0612d88af8e91662820c6a4fa
https://doi.org/10.1016/j.gloplacha.2011.04.006
https://doi.org/10.1016/j.gloplacha.2011.04.006
Publikováno v:
Chemical Geology. 258:242-250
A continuous 60-year record (1938–1998) of stable isotope compositions of carbon and oxygen, as well as trace metal (Mg, Sr, Ba) concentrations in a laminated calcite crust precipitated in a short artificial tunnel on a non-equilibrium groundwater-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9d3a7c543cc77ea13660f7725cad4a2
https://doi.org/10.1016/j.chemgeo.2008.10.013
https://doi.org/10.1016/j.chemgeo.2008.10.013
Autor:
Juan A. Vázquez-Navarro
Publikováno v:
Quaternary International. :517-518
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5ff4d73eee3d683d7e27235b7b46508
https://doi.org/10.1016/j.quaint.2012.08.1791
https://doi.org/10.1016/j.quaint.2012.08.1791
Autor:
Juan A. Vázquez-Navarro
Publikováno v:
Quaternary International. :518
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cfc8a40f175d967a1f5e26843c3dd2e0
https://doi.org/10.1016/j.quaint.2012.08.1792
https://doi.org/10.1016/j.quaint.2012.08.1792