Integrated Reservoir Petrophysical Characterization and 3D Modeling: a Deep-Water Turbidite Reservoir Case Study

2008 ◽  
Author(s):  
Livio Ruvo ◽  
Mirko Calderoni ◽  
Marco Cesaro ◽  
Franco Fonnesu ◽  
Ilario Franco ◽  
...  
Keyword(s):  
Author(s):  
L. Ruvo ◽  
M. Calderoni ◽  
M. Cesaro ◽  
F. Fonnesu ◽  
I. Franco ◽  
...  
Keyword(s):  

2014 ◽  
Author(s):  
Catherine Sugden ◽  
William Bacon ◽  
Oscar Gabaldon ◽  
Jose Umberto Arnaud Borges ◽  
Cristiane Maraviha Soares ◽  
...  

Minerals ◽  
2018 ◽  
Vol 8 (7) ◽  
pp. 271 ◽  
Author(s):  
Michael Zhdanov ◽  
Fouzan Alfouzan ◽  
Leif Cox ◽  
Abdulrahman Alotaibi ◽  
Mazen Alyousif ◽  
...  

2017 ◽  
Vol 68 (5) ◽  
pp. 403-418 ◽  
Author(s):  
Ján Soták ◽  
Zuzana Pulišová ◽  
Dušan Plašienka ◽  
Viera Šimonová

Abstract The Súľov Conglomerates represent mass-transport deposits of the Súľov-Domaniža Basin. Their lithosomes are intercalated by claystones of late Thanetian (Zones P3 - P4), early Ypresian (Zones P5 - E2) and late Ypresian to early Lutetian (Zones E5 - E9) age. Claystone interbeds contain rich planktonic and agglutinated microfauna, implying deep-water environments of gravity-flow deposition. The basin was supplied by continental margin deposystems, and filled with submarine landslides, fault-scarp breccias, base-of-slope aprons, debris-flow lobes and distal fans of debrite and turbidite deposits. Synsedimentary tectonics of the Súľov-Domaniža Basin started in the late Thanetian - early Ypresian by normal faulting and disintegration of the orogenic wedge margin. Fault-related fissures were filled by carbonate bedrock breccias and banded crystalline calcite veins (onyxites). The subsidence accelerated during the Ypresian and early Lutetian by gravitational collapse and subcrustal tectonic erosion of the CWC plate. The basin subsided to lower bathyal up to abyssal depth along with downslope accumulation of mass-flow deposits. Tectonic inversion of the basin resulted from the Oligocene - early Miocene transpression (σ1 rotated from NW-SE to NNW-SSE), which changed to a transpressional regime during the Middle Miocene (σ1 rotated from NNE-SSW to NE-SW). Late Miocene tectonics were dominated by an extensional regime with σ3 axis in NNW-SSE orientation.


Author(s):  
A. Rodriguez

In three-dimensional models of urban historical reconstruction, missed contextual architecture faces difficulties because it does not have much written references in contrast to the most important monuments. This is the case of Merida, Yucatan, Mexico during the Colonial Era (1542-1810), which has lost much of its heritage. An alternative to offer a hypothetical view of these elements is a typological - parametric definition that allows a 3D modeling approach to the most common features of this heritage evidence.


2015 ◽  
Vol 59 ◽  
pp. 268-285 ◽  
Author(s):  
Amandine Prélat ◽  
David M. Hodgson ◽  
Mark Hall ◽  
Christopher A.-L. Jackson ◽  
Carol Baunack ◽  
...  
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2018 ◽  
Vol 11 (5) ◽  
pp. 1973-1976 ◽  
Author(s):  
Ahmet Suad Toprak ◽  
Nizar Polat ◽  
Murat Uysal
Keyword(s):  

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