Zobrazeno 1 - 10
of 40
pro vyhledávání: '"E. Remacha"'
Publikováno v:
Journal of Micropalaeontology, Vol 43, Pp 55-68 (2024)
This study presents the first detailed data on calcareous nannofossil assemblages from the Sabiñánigo Sandstone Formation in the Jaca Basin (central south Pyrenees). This formation is mainly composed of deltaic and outer-shelf sediments. These sili
Externí odkaz:
https://doaj.org/article/bc0308be2d8043d7b1f09f0351f7a745
Akademický článek
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Publikováno v:
Journal of the Geological Society. 176:1182-1190
We investigate how sedimentary systems respond to tectonic uplift during the last stages of infilling of a foreland basin. Massive conglomeratic deposits characterize the last stage of basin fill in the Jaca basin, the western portion of the South Py
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec1fa1806b5e3a865c0d3d2d67f8a083
https://doi.org/10.1144/jgs2018-228
https://doi.org/10.1144/jgs2018-228
Supplementary material 3: Full detrital zircon U–Pb spectra from 0 Ma to 3500 Ma, displayed as kernel density estimators (KDE) and histograms (Vermeesch, 2012). Nonadaptive KDE bandwidth of 8 Ma, histogram bin width of 20 Ma.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d653d6a0d8ca3c0e2295ba1278c54e9
Supplementary material 1: Extended Zircon U–Pb LA–ICP–MS methodology.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2c3c8e30aaf1d9fb0311484bbbb6865f
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
The Eocene clastic systems of the Jaca foreland Basin (southern Pyrenees) allow us to identify changes in sediment composition through time. We provide new data on sediment composition and sources of the northern Jaca basin, whose stratigraphic evolu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d8e45e4b2df05be2070b5e6c942ba179
https://doi.org/10.1016/j.crte.2015.10.005
https://doi.org/10.1016/j.crte.2015.10.005
Publikováno v:
Cretaceous Research. 57:414-427
A detailed petrological study has been performed for the end-Cretaceous clastic deposits of the southern Pyrenees. Provenance results indicate that the Maastrichtian systems from both the Ager and the Vallcebre synclines show compositional features t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1f4d34edd6861468baeaf3cee2d449a
https://doi.org/10.1016/j.cretres.2015.09.010
https://doi.org/10.1016/j.cretres.2015.09.010
Publikováno v:
Spanish Journal of Palaeontology, Vol 34, Iss 2, Pp 229-240 (2021)
The calcareous nanoplankton is studied from the base of the turbidite systems of the Upper Hecho Group (Jaca Basin, middle Eocene of the South-central Pyrenean Basin) up to the Gracionepel instabilities, within the Larres slope Marls. This new chrono
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a2aa0cf06d7be3b84e3fd9ace2ca50b
https://doi.org/10.7203/sjp.34.2.16096
https://doi.org/10.7203/sjp.34.2.16096
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
In the northern Jaca basin (Southern Pyrenees), the replacement of deep-marine by terrestrial environments during the Eocene records a main drainage reorganization in the active Pyrenean pro-wedge, which leads to recycling of earlier foreland basin s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f47dad2db034ac22aeea0a12b3efe8a0
http://hdl.handle.net/10261/157189
http://hdl.handle.net/10261/157189
Publikováno v:
Marine and Petroleum Geology. 25:255-270
Optimum hydrocarbon recovery from clastic reservoirs depends on the depth of our knowledge of the detailed architecture of intercalated shaly baffles and barriers. In the case of deep marine turbidite fields, the usual investigation methods are often
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98634e981751047b9dbb73aabc32457f
https://doi.org/10.1016/j.marpetgeo.2007.07.003
https://doi.org/10.1016/j.marpetgeo.2007.07.003