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Guangrong Peng, Pei Liu, Weitao Chen, Zhensheng Li, Xiaomeng Wang, Zhiwei Zhang, Xuanlong Shan and Guoli Hao
The Pearl River Mouth Basin (PRMB) is located in the northern part of the South China Sea. The Palaeogene Wenchang Formation (Fm) was formed at the rift stage and contains the main source rocks. The migration of Wenchang subsidence centres in the western...
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Kevin C. Hill, Gareth T. Cooper, Agnes Pokondepa, Peter Essy, Thiwaporn Phonsit and Mark Haydon
The Porgera Transfer Zone (PTZ) is a major crustal and probably lithospheric structure across Papua New Guinea recording >50 km offset of ophiolites and very different patterns of geology and topography on either side. In the Late Jurassic, the PTZ proba...
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Joschka Röth and Ralf Littke
The Cooper subregion within the central Eromanga Basin is the Swiss army knife among Australia?s sedimentary basins. In addition to important oil and gas resources, it hosts abundant coal bed methane, important groundwater resources, features suitable co...
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Salvatore Gambino, Giovanni Barreca, Valentina Bruno, Giorgio De Guidi, Carmelo Ferlito, Felix Gross, Mario Mattia, Luciano Scarfì and Carmelo Monaco
Offshore data in the western Ionian Sea indicate that the NW?SE-trending dextral shear zone of the Alfeo-Etna Fault System turns to the N?S direction near the Ionian coastline, where the extensional Timpe Fault System is located. Morpho-structural data s...
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Paola Cianfarra, Marcos Roberto Pinheiro, Fernando Nadal Junqueira Villela and Francesco Salvini
We present the effect of neotectonics in intracratonic settings as revealed by the surface, brittle deformation associated to a regionally-sized shear corridor, which affects Southeastern Brazil. The deformation zone is characterized by the presence of n...
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Zhan Zhao, Jingtao Liu, Wenlong Ding, Ruiqiang Yang and Gang Zhao
Fault damage zone has an important influence on subsurface fluid flow and petrophysical properties. Therefore, it is of great significance to study the characteristics of fault damage zone for oil and gas development of ultra-deep carbonate formation. Th...
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Guangxin Zhou, Qian Sheng, Zhen Cui, Tianqiang Wang and Yalina Ma
Knowledge from historical earthquake events indicates that a submarine tunnel crossing active strike-slip faults is prone to be damaged in an earthquake. Previous studies have demonstrated that the flexible joints are an effective measure for a submarine...
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Jose Araya,Gregory P. De Pascale,Rodrigo Mardel,Sergio A. Sepúlveda
Pág. 529 - 545
Understanding the location and nature of Quaternary active crustal faults is critical to the reduction of both fault rupture and strong ground motions hazards in built environments. Recent work along the San Ramón Fault (SRF) demonstrates that crustal se...
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Martin D. Clark, Elizaveta Kovaleva, Matthew S. Huber, Francois Fourie and Chris Harris
Better characterization features borne from long-term crustal modification processes is essential for understanding the dynamics of large basin-forming impact structures on Earth. Within the deeply eroded 2.02 Ga Vredefort Impact Structure in South Afric...
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Stella M. Moreiras,Laura B. Giambiagi,Silvana Spagnotto,Silvina Nacif,Jose Mescua,Rafael Toural Dapoza
Pág. 342 - 361
Current active front of the Central Andes comprises part of the western piedmont of the city of Mendoza, where more than 800,000 people are established. Despite this, a comprehensive study of active faults mainly as potential seismogenic sources is lacki...
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