Zobrazeno 1 - 10
of 23
pro vyhledávání: '"T. Geel"'
Autor:
T. Geel
Publikováno v:
Estudios Geologicos, Vol 52, Iss 5-6, Pp 211-230 (1996)
La Sierra Espuña está situada al margen norte de la Zona Interna en la parte oriental de las Cordilleras Béticas y forma parte del Complejo Maláguide no metamórfico. Análisis paleontológico y sedimentológico de sedimentos de edad Eoceno al Aq
Externí odkaz:
https://doaj.org/article/c6f54d00132f406caabd33c9a66b2f61
Autor:
T Geel
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 155:211-238
The functional morphology and life style of foraminifers can be used to determine their former position on the platform and to detect upwards shallowing and deepening trends in sedimentary sequences. The sequential analysis of the Palaeogene platform
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55d4e5b40e59f993f4daf32181af3ecc
https://doi.org/10.1016/s0031-0182(99)00117-0
https://doi.org/10.1016/s0031-0182(99)00117-0
Autor:
Jens Lehmann, T. Geel, R. W. Scott, Adrian Immenhauser, L.J.A. Bolder-Schrijver, Wolfgang Schlager, S. van der Gaast, Stephen J. Burns
Publikováno v:
Journal of Sedimentary Research, 69, 434-446. SEPM Society for Sedimentary Geology
Immenhauser, A M, Schlager, W, Burns, S J, Scott, R W, Geel, T, Lehmann, J, van der Gaast, S & Bolder-Schrijver, L J A 1999, ' Late Aptian to Late Albian sea-level fluctuations constrained by geochemical and biological evidence (Nahr Umr Fm, Oman). ', Journal of Sedimentary Research, vol. 69, pp. 434-446 . https://doi.org/10.2110/jsr.69.434
Immenhauser, A M, Schlager, W, Burns, S J, Scott, R W, Geel, T, Lehmann, J, van der Gaast, S & Bolder-Schrijver, L J A 1999, ' Late Aptian to Late Albian sea-level fluctuations constrained by geochemical and biological evidence (Nahr Umr Fm, Oman). ', Journal of Sedimentary Research, vol. 69, pp. 434-446 . https://doi.org/10.2110/jsr.69.434
The Aptian to Albian interval of the vast Arabian Platform was studied in northern Oman (Nahr Umr Formation) for its paleoceanographic and sea-level record. The sections indicate seven transgressive-regressive cycles overprinted by small-scale sea-le
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c8f40057d7003c3c58ed02e968ad6353
https://research.vu.nl/en/publications/7d83a292-a825-4b47-96d5-8946675b7382
https://research.vu.nl/en/publications/7d83a292-a825-4b47-96d5-8946675b7382
Autor:
T. Geel, Th.B. Roep
Publikováno v:
Geologie en Mijnbouw (Geology and Mining). 77:39-61
The Velez Rubio Corridor and the area northwest of the Sierra Espuna are located on the Internal-External Zone Boundary. The External Zone is represented by the Southern Subbetic, the most basinward part of the former passive margin of Iberia, the In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d6f5bb877fe307ba64727bf8940995d
https://doi.org/10.1023/a:1003438421905
https://doi.org/10.1023/a:1003438421905
Autor:
T. Geel
Publikováno v:
Basin Research. 7:313-336
The Alicante region, situated at the intersection of major Western Mediterranean structural units, is unique in possessing a complete marine Oligocene to early Miocene record of both platform and slope deposits. Detailed analysis of three selected pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::447867ce4d78bbb7f3b2b74c6dd7fb93
https://doi.org/10.1111/j.1365-2117.1995.tb00120.x
https://doi.org/10.1111/j.1365-2117.1995.tb00120.x
Publikováno v:
Sedimentary Geology. 75:223-239
The paper concerns the Miocene deposits of the Alicante region (SE Spain) which forms part of the Prebetic and Intermediate units, representing the former southern passive margin of the Iberian continent. From the Late Jurassic up to the Miocene, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::29d54a7c8bf9f3e148c818217d3e3e81
https://doi.org/10.1016/0037-0738(92)90094-8
https://doi.org/10.1016/0037-0738(92)90094-8
Autor:
T. Geel
Publikováno v:
Estudios Geológicos. 52
The Sierra Espuna is situated at the northern edge of the Internal Zone in the eastern Betic Cordilleras and is part of the unmetamorphosed Malaguide Complex. Palaeontological and sedimentological analysis of the Eocene to Aquitanian sediments on the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46d15b6a28fee10b0b8904be976805b4
https://doi.org/10.3989/egeol.96525-6267
https://doi.org/10.3989/egeol.96525-6267
Publikováno v:
Geological Society of America Bulletin. 103:1504
Rapid sea-level changes are generally interpreted in terms of glacio-eustasy, but they can also be explained by the lithospheric motions associated with changes in intra-plate stress. In eastern Spain, latest Senonian-Paleocene time was characterized
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcb4e4eb58bb3b71888c046fc308aec6
https://doi.org/10.1130/0016-7606(1991)103<1504:eotpco>2.3.co
https://doi.org/10.1130/0016-7606(1991)103<1504:eotpco>2.3.co
Publikováno v:
Geologische Rundschau. 53:233-259
The stratigraphy of Betic of Malaga and of Subbetic near Velez Rubio is given. No major tectonic movement took place between Paleozoic and Oligo-Miocene in the area of deposition of the Betic of Malaga and neighbourhood. The geology and formations of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::350edfb547085c1ed8b6861a45f98391
https://doi.org/10.1007/bf02040749
https://doi.org/10.1007/bf02040749