Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Luciano P. Magnavita"'
Autor:
Sabrina Helena Diniz Gilaberte Bezerra, Luciano P. Magnavita, Renato Oscar Kowsmann, Nolan Maia Dehler, Geise de Santana dos Anjos Zerfass, Marcos Nobrega, Juliana Andrade Iemini, Antonio Fernando Menezes Freire, Seirin Shimabukuro, Dennis J. Miller, Adriano R. Viana
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 146:45-52
An international research cruise named Iata-Piuna took place on the Sao Paulo Plateau on May 2013 in the Campos and Espirito Santo basins, off Brazil. The cruise was carried ou on board the research vessel (R/V) Yokosuka that hosts the human operated
Publikováno v:
Journal of Structural Geology. 25:1263-1279
The Jeremoabo fault, located in the Early Cretaceous Reconcavo–Tucano Rift, northeastern Brazil, represents an example of transfer fault. A field-based structural analysis along 20 km of exposures revealed an E–W-trending and steeply dipping reve
Publikováno v:
AAPG Bulletin. 87:1123-1144
Release faults are rift cross faults, which develop to accommodate the variable displacements of the hanging-wall block along the strike of normal faults. Release faults are nearly perpendicular or obliquely oriented to the strike of the normal fault
Autor:
Caesar Augusto Rigoti, Pedro Victor Zalán, Luciano P. Magnavita, Maria do Carmo Garcia Severino, Adriano R. Viana, João Alberto Bach de Oliveira
Publikováno v:
Marine and Petroleum Geology.
Autor:
Luciano P. Magnavita, Dario Chiossi, Paul F. Green, Peter Japsen, Augusto J. Pedreira, Johan M. Bonow, Peter R. Cobbold, Ragnhild Lilletveit
Publikováno v:
Geological Society of America Bulletin
Geological Society of America Bulletin, 2012, 124 (5-6), pp.800-816. ⟨10.1130/B30515.1⟩
Geological Society of America Bulletin, Geological Society of America, 2012, 124 (5-6), pp.800-816. ⟨10.1130/B30515.1⟩
Geological Society of America Bulletin, 2012, 124 (5-6), pp.800-816. ⟨10.1130/B30515.1⟩
Geological Society of America Bulletin, Geological Society of America, 2012, 124 (5-6), pp.800-816. ⟨10.1130/B30515.1⟩
International audience; It is a common assumption that elevated passive continental margins have remained high since rifting and breakup. Here, we show that the Atlantic margin of NE Brazil has under gone a more complex history. Our synthesis of geol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::47628332ba2432bb01f2f04f2a9ee183
https://hal-insu.archives-ouvertes.fr/insu-00705178
https://hal-insu.archives-ouvertes.fr/insu-00705178
The Reconcavo basin forms the southern end of the inland Reconcavo-Tucano-Jatoba rift system, whose propagation to the north was arrested by the transverse Pernambuco shear zone, causing final rifting and continental break-up to propagate along an al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::163f7a5011e9db1cde88f988f2cd08d7
https://doi.org/10.1016/b978-0-444-56356-9.00014-6
https://doi.org/10.1016/b978-0-444-56356-9.00014-6
Publikováno v:
Tectonics. 13:367-388
The Reconcavo-Tucano-Jatoba (RTJ) Rift and many other smaller sedimentary basins in northeast Brazil formed during South Atlantic rifting and were subsequently uplifted and exhumed so that Albian marine sediments are now located up to 800 m above sea
Publikováno v:
AAPG Bulletin. 79
A geometric and depositional model is proposed to explain the tectonic and sedimentary evolution of the main border of the Reconcavo basin. The architecture of the rift margin is characterized by a rift border system constituted by (1) a master fault
Publikováno v:
Revista Brasileira de Geociências. 18:222-230
Until recently, the Lower Cretaceous Reconcavo-Tucano-Jatoba Rift was interpreted as being a system of basins connected since the beginning of rifting and filled by a fluvio-deltaic-lacustrine system which prograded from north to south. In this work,