Encontrados 4 documentos, a visualizar página 1 de 1

Ordenado por Data

Goldra: premier gisement karstique en Algarve, faune et industries

Antunes, M. T.; Manuppella, G.; Mein, P.; Zbyszewski, G.

A bone breccia from Goldra, near Loulé, is studied. It corresponds to the infilling of a karst depression, consisting of: rather worn and probably transported dolomite pebbles at the bottom; accumulations of frequently burnt bone scraps, much broken and with acute edges (no transport), certainly debris of human food, suggesting habitat level (s); in association with the former, stone (flint, quartz, quartzite, ...

Data: 2008   |   Origem: Repositório Institucional da UNL

Contribuição para a datação do conglomerado de Odeáxere

Manuppella, G.; Rocha, R. B.

According to P. Choffat, Odeáxere conglomerate was Oxfordian in age, and would represent the unconformity between Malm and Dogger. Choffat's opinion was based exclusively in a lithological comparison with conglomerates from Arrábida; these conglomerates are now reported to the Dogger, as they are intercalated between beds with Timidonella sarda. However, in the mesogean realm, the stratigraphical position of T....

Data: 2008   |   Origem: Repositório Institucional da UNL

Estratigrafia do Caloviano do Algarve oriental

Manuppella, G.; Marques, B.; Rocha, R. B.

The comparative study of the Callovian sections in eastern Algarve allowed us to demonstrate that the discontinuity surface at the base of Malm lies always over the Lower-Callovian, as opposite to what happens in western Algarve; the Bathonian-Callovian transition, continuous in western Algarve (Mareta beach) is marked, in eastern Algarve, by a generalised discontinuity of variable vertical extention. It is ver...

Data: 2008   |   Origem: Repositório Institucional da UNL

Aspectos gerais da tectónica alpina no Algarve

Kullberg, J. C.; Pais, João; Manuppella, G.

The study of the tectonic strutures affecting the mesozoic and cenozoic deposits of Algarve's basin allows us to recognize the following phases of the Alpine orogeny: Jurassic (Upper Triassic at least)-Lower Cretaceous N-S distension; N-S compression during the setting-up of the Monchique syenite dome at the uppermost Cretaceous; Paleogene compression (?) (only locally? - at the Albufeira salt dome); Lower Mioc...

Data: 1992   |   Origem: Repositório Institucional da UNL

4 Resultados

Texto Pesquisado

Refinar resultados

Autor









Data



Tipo de Documento


Recurso


Assunto















    Financiadores do RCAAP

Fundação para a Ciência e a Tecnologia Universidade do Minho   Governo Português Ministério da Educação e Ciência Programa Operacional da Sociedade do Conhecimento União Europeia