Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Nivaldo Destro"'
Publikováno v:
Interpretation. 7:SH19-SH31
The Sergipe-Alagoas Basin, situated in the north-east Brazilian margin, has a long tradition of oil and gas production and the presence and distribution of evaporites play an important role in petroleum systems in the basin. However, little research
Publikováno v:
Journal of South American Earth Sciences. 83:37-54
Autor:
Nivaldo Destro
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Journal of Structural Geology. 32:1783-1791
It is assumed that deformation bands may compartmentalize aquifers or hydrocarbon reservoirs because these low-permeability structures may behave as barriers to fluid flow. To address the question whether there is, at a reservoir scale, hydraulic con
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:
Nivaldo Destro
Publikováno v:
Journal of Structural Geology. 17:615-629
Two types of cross faults are herein recognized: transfer faults and the newly termed release faults. Transfer faults form where cross faults connect distinct normal faults and horizontal displacements predominate over vertical ones. In contrast, rel
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:
Journal of Structural Geology. 16:35-45
Reactivation of Proterozoic ductile shear zones is often difficult to document because of the lack of conclusive evidence. However, the reactivation of a Proterozoic age ductile shear zone along the northeastern extremity of the Transbrazilian Lineam