Zobrazeno 1 - 10
of 66
pro vyhledávání: '"Cristina Persano"'
Publikováno v:
Scottish Geographical Journal. 138:382-388
Speleothems, secondary cave carbonates, are valuable archives for reconstructing paleoclimate and relative sea-level changes where the caves are in coastal locations. Unlike the typical speleothems found in carbonate caves, speleothems were recently
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c70ce19d64af386f5a906b636cf6286e
https://doi.org/10.5194/egusphere-egu23-152
https://doi.org/10.5194/egusphere-egu23-152
Deep (> 500 m below ground) geothermal energy is generated by heat sources within the Earth, including unusually high lithospheric basal heat flow and/or intrusive bodies rich in radioactive isotopes, that heat the surrounding rocks and aquifers. Thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42a7230f95842940d3d3e281c076a969
https://doi.org/10.5194/egusphere-egu23-17462
https://doi.org/10.5194/egusphere-egu23-17462
Autor:
Diego Alves de Oliveira, Cristina Helena Ribeiro Rocha Augustin, Paulo Roberto Antunes Aranha, Tom Dargie, Cristina Persano, Rubens Martins Moreira
Wetlands represent an excellent example of the interface between lithosphere, atmosphere, and hydrosphere. Despite being distributed throughout the planet, the pace of their destruction has increased, especially since the 1970s. In tropical regions,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4c5208232f8ab0dce3865b4733c96b6
https://doi.org/10.5194/icg2022-248
https://doi.org/10.5194/icg2022-248
Publikováno v:
Earth Surface Dynamics, Vol 9, Pp 167-181 (2021)
Many mountain ranges survive in a phase of erosional decay for millions of years following the cessation of tectonic activity. Landscape dynamics in these post-orogenic settings have long puzzled geologists due to the expectation that topographic rel
The Midland Valley Basin of Scotland (MVS) is a major NE-SW trending, fault-bounded sedimentary basin in central Scotland, UK, comprised predominantly of Carboniferous and Devonian sedimentary rocks. Changing palaeo-environments of the MVS produced a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5960603dedd0f7e1b65a91877a58c5e7
https://doi.org/10.5194/egusphere-egu22-8433
https://doi.org/10.5194/egusphere-egu22-8433
Autor:
Weiwei Xue, Yani Najman, Xiumian Hu, Cristina Persano, Finlay M. Stuart, Wei Li, Anlin Ma, Ying Wang
Publikováno v:
Tectonics. 41
Much of the interior of the Tibetan Plateau is characterized by internal drainage, low relief topography, and high altitude. How and when this landscape formed is controversial. In this study, we use new zircon U-Pb data and low-temperature thermochr
Autor:
Cristina Persano, Diego Alves de Oliveira, Cristina Helena Ribeiro Rocha Augustin, Trevor Hoey
The presence of wetlands as a result of local fluvial and hydrological conditions constitutes a frequently observed feature of such rivers. Therefore, they are important elements of the basin, because besides functioning as buffer zones for CO2 and s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c069258fa375589e250f1dbe231f89a8
https://doi.org/10.5194/egusphere-egu21-9075
https://doi.org/10.5194/egusphere-egu21-9075
Knowledge of the geological history of the Tibetan plateau is critical to understanding crustal deformation process, and the plateau’s influence on climate. However, the timing of Tibetan plateau development remains controversial. The Nima Basin al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eece39aa3c8fe5cd5d87c09d3a6e6ef1
https://doi.org/10.5194/egusphere-egu2020-5082
https://doi.org/10.5194/egusphere-egu2020-5082