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Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Fuerteventura and Lanzarote islands were created by volcanic processes that took place on the western margin of the triassic rift basin developed during the initial opening of the Central Atlantic. Thick syn-rift deposits consisting mainly of salt-an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::13705c3b5049da71ec3145ea4525b68a
http://hdl.handle.net/10272/9382
http://hdl.handle.net/10272/9382
Fuerteventura and Lanzarote islands were created by volcanic processes that took place on the western margin of the triassic rift basin developed during the initial opening of the Central Atlantic. Thick syn-rift deposits consisting mainly of salt-an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::13705c3b5049da71ec3145ea4525b68a
Autor:
Martínez del Olmo, W.
Wells drilled for hydrocarbon exploration provide plentiful lithostratigraphic information which, combined with the flooding and shallowing parasequences obtained from well log interpretation, allow the characterization of System Tracts and Depositio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::2fa02aaef2eddf7d3458641487ffa56c
https://hdl.handle.net/10272/11361
https://hdl.handle.net/10272/11361
Autor:
Martínez del Olmo, W.
The Scythian to HeUangian sedimentary record of the Eastern Spain includes an initial rift-type supersequence (Buntsandstein) and four Depositional Sequences (Muschelkalk-Keuper). Within the rift tectofacies the tectonic influence just charactize a c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::4bfc81d811fc166b151aaac35b9ad47f
Autor:
Martínez del Olmo, W.
40 System Tracts have been characterized from surface and subsurface data obtained from Jurassic platform and slope facies on southeastern Spain. With the exception of the initial Depositional Sequence (Lower Liassic) which was controlled by a disten
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::d69cf5e7a48eb95ab48186d44638a788
https://hdl.handle.net/10272/11386
https://hdl.handle.net/10272/11386
Autor:
Martínez del Olmo, W.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
40 System Tracts have been characterized from surface and subsurface data obtained from Jurassic platform and slope facies on southeastern Spain. With the exception of the initial Depositional Sequence (Lower Liassic) which was controlled by a disten
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::d69cf5e7a48eb95ab48186d44638a788
http://hdl.handle.net/10272/11386
http://hdl.handle.net/10272/11386
Autor:
Martínez del Olmo, W.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Scythian to HeUangian sedimentary record of the Eastern Spain includes an initial rift-type supersequence (Buntsandstein) and four Depositional Sequences (Muschelkalk-Keuper). Within the rift tectofacies the tectonic influence just charactize a c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::4bfc81d811fc166b151aaac35b9ad47f
http://hdl.handle.net/10272/11385
http://hdl.handle.net/10272/11385
Autor:
Martínez del Olmo, W.
The geometry and the areas of erosion/deposition of the System Tracts of which Depositional Sequences are made up of, and the ways in which the fatter are superimposed, are controlled by several factors. These factors can be considered to be grouped
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::82d69a2bbfb55abe4075195505345785
https://hdl.handle.net/10272/11434
https://hdl.handle.net/10272/11434
Autor:
Martínez del Olmo, W.
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Surface and subsurface data obtained from Cretaceous platform facies at southeastern Spain have allowed the characterization of 55 System Tracts. The sedimentary architecture observed from the 27 Depositional Sequences identifiedI indicates that they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::b04c02e4055d9f718a9ed3430bd620e5
http://hdl.handle.net/10272/11388
http://hdl.handle.net/10272/11388