Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Mendes, M. H."'
Autor:
CAETANO, E. M.1 ericami468@gmail.com, MENDES, M. H. F.1 marcelohfmendes2@gmail.com, NOGUEIRA, F. C.1 francielle.nogueira@ufop.edu.br, MENDES, J. J.1 jefferson.mendes@ifmg.edu.br, PEREIRA, C. A.1 carlos.ii@ufop.edu.br, SILVA, F. L.1 fabiane.silva@uemg.br
Publikováno v:
HOLOS. 2023, Vol. 4, p1-18. 18p.
The dolerite samples studied in this work are part of drilling cores, obtained during exploration campaigns by the Ncondezi Coal Company, in the prospect area 805L, located at NE of Moatize, Tete Province, Mozambique. The dolerite bodies are intrusiv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2292::3c2834d0fc0fe234a337eddfc037fd77
http://hdl.handle.net/10773/21159
http://hdl.handle.net/10773/21159
Publikováno v:
Estudios Geologicos, Vol 66, Iss 1, Pp 25-34 (2010)
The Reguengos de Monsaraz pluton is a late to post-tectonic Variscan intrusion occurring in the Ossa Morena Zone (Iberian Variscan Chain). The dominant lithological types are tonalites and granodiorites, but the internal area of the massif is compose
Publikováno v:
CIÊNCIAVITAE
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Scopus-Elsevier
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Scopus-Elsevier
The Lalezar granitoids crop out within volcanic successions of the Urumieh-Dokhtar Magmatic Assemblage (UDMA). These granitoids have a range from gabbro-diorites to granites in composition. The mineral compositions of the most felsic rocks are charac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3317855f68f52a70aac88196126998ba
http://hdl.handle.net/10773/15554
http://hdl.handle.net/10773/15554
Akademický článek
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Akademický článek
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Autor:
Almeida, B., Seixas, T. M., Mendes, M. H., Ferro, M. C., Salgueiro da Silva, M. A., Santos, J. F., Almeida, F., Diogo, Z., Lopes, A. B., Vieira, J.
The research on interplanetary materials such as comets, meteors or meteorites contributes to understand the origin and evolution of our Solar System. They provide highly valuable information on the relation between the conditions of formation and th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2292::21ecaf9cfb07e22c426c1c4f04db9ecb
http://hdl.handle.net/10773/11627
http://hdl.handle.net/10773/11627
Autor:
Seixas, T. M., Silva, M. A. S., Almeida, F., Diogo, Z., Mendes, M. H., Santos, J. F., Vieira, J. M., Marques, M.
Meteorites are remnants of geological processes that occurred in our Solar System. Properly analyzed, the bulk composition, mineralogy, and petrology of meteorites can be used to constrain planet formation processes. Moreover, the laboratorial charac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2292::7595bfb58caeff6acee15f6df72da764
http://hdl.handle.net/10773/9358
http://hdl.handle.net/10773/9358
Santo Antão Island is the northernmost island of the Cape Verde Archipelago that is located in the Atlantic Ocean between 17º 13’N-14º 48’N and 22º 42’W-25º 22’W. The genesis of this Archipelago is explained by the activity of a hot-spot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2019::2fee2287af4af6da7b0de9a5dd852dd1
https://hdl.handle.net/10400.9/3524
https://hdl.handle.net/10400.9/3524
Publikováno v:
CIÊNCIAVITAE
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Os xenólitos ultramáficos, existentes em lavas basálticas alcalinas/nefeliníticas da Ilha de Santo Antão (Cabo Verde), incluem uma série harzburgítica e uma série dunítica/wehrlítica; a série harzburgítica apresenta características textu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cdd9afa7a7bba85fc2fa75405caf46a9
https://hdl.handle.net/10400.9/860
https://hdl.handle.net/10400.9/860