Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Arostegui García, Javier"'
Achneliths generated in lava fountains of the Campo de Calatrava Volcanic Field (Ciudad Real, Spain)
Autor:
Carracedo Sánchez, Manuel, Sarrionandia Eguidazu, Fernando, Arostegui García, Javier, Gil Ibarguchi, José Ignacio
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
We describe and discuss the origin of achneliths that occur within ash and lapilli tephra emitted by the Las Herrerías volcano of the Campo de Calatrava Volcanic Field (CCVF, Ciudad Real, Spain). These ash-size pyroclasts exhibit fluidal shapes (sph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8a7f83d06d16b5467cb343da421d449b
https://hdl.handle.net/10272/8776
https://hdl.handle.net/10272/8776
Autor:
Carracedo Sánchez, Manuel, Sarrionandia Eguidazu, Fernando, Gil Ibarguchi, José Ignacio, Arostegui García, Javier
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The Cabezo Segura volcano is located in the central part of the Calatrava Volcanic Province. Some deposits of this volcano are formed by singular spherical lapilli and bombs. These lapilli and bombs are the result of welding of ash and fine-grained l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::24e6450326987a81c5cc265e5c31a085
http://hdl.handle.net/10272/8110
http://hdl.handle.net/10272/8110
Autor:
Carracedo Sánchez, Manuel, Sarrionandia Eguidazu, Fernando, Gil Ibarguchi, José Ignacio, Arostegui García, Javier
The Cabezo Segura volcano is located in the central part of the Calatrava Volcanic Province. Some deposits of this volcano are formed by singular spherical lapilli and bombs. These lapilli and bombs are the result of welding of ash and fine-grained l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::24e6450326987a81c5cc265e5c31a085
https://hdl.handle.net/10272/8110
https://hdl.handle.net/10272/8110
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The sandstones of the Gordexola Formation were studied using petrography, cathodoluminescence, electronic microprobe, SEM, and C and O isotopic relations. A diagenetic sequence was inferred from medium to late stages. The processes that affected sand
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::6dd70c54252174aadb2e68b1f4d172d9
http://hdl.handle.net/10272/10582
http://hdl.handle.net/10272/10582
The sandstones of the Gordexola Formation have been petrologically and geochemically studied. The averageofQ(= 57%), FdK+Plag(= 6%) and rock fragments (= 4%) in sandstones was plotted against the Dickinson et al. (1983) and Suttner and Basu (1981) di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::5ef5d800f3efe7896a043047a4eecfb5
https://hdl.handle.net/10272/10581
https://hdl.handle.net/10272/10581
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The sandstones of the Gordexola Formation have been petrologically and geochemically studied. The averageofQ(= 57%), FdK+Plag(= 6%) and rock fragments (= 4%) in sandstones was plotted against the Dickinson et al. (1983) and Suttner and Basu (1981) di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::5ef5d800f3efe7896a043047a4eecfb5
http://hdl.handle.net/10272/10581
http://hdl.handle.net/10272/10581
The sandstones of the Gordexola Formation were studied using petrography, cathodoluminescence, electronic microprobe, SEM, and C and O isotopic relations. A diagenetic sequence was inferred from medium to late stages. The processes that affected sand
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::6dd70c54252174aadb2e68b1f4d172d9
https://hdl.handle.net/10272/10582
https://hdl.handle.net/10272/10582
The fades organization of the Gordexola Formation (lower to middle Albian) has been studied in a sector along the south limb of Bilbao antidinorium. Black shales deposited in basin environments constitute the background facies. The basal and intermed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::91e2a263dffc8525b296cf199a0f312b
https://hdl.handle.net/10272/12176
https://hdl.handle.net/10272/12176
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The fades organization of the Gordexola Formation (lower to middle Albian) has been studied in a sector along the south limb of Bilbao antidinorium. Black shales deposited in basin environments constitute the background facies. The basal and intermed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::91e2a263dffc8525b296cf199a0f312b
http://hdl.handle.net/10272/12176
http://hdl.handle.net/10272/12176
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Three diferent parameters of ilites from the unconformable Buntsandstein of the Cinco Villas, Alduides and Oroz-Betelu basque Paleozoic massifs can be interpreted as characteristic of either the iberian or european plates. The Leiza Fault, which is t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e944b7807a1c1c7bcd77ff921e913ccc