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Zhen Yang, Guangxue Zhang, Shiguo Wu, Youhua Zhu, Cong Wu, Li Zhang, Songfeng Liu, Wei Yan, Ming Sun, Yaoming Zhang, Xuebin Du and Chenlu Xu
The newly collected seismic data and the existing drilling data provide a good opportunity to better understand the carbonate platform distribution characteristics and the hydrocarbon resource potential in the Xisha sea area of the South China Sea. Based...
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Wenbo Du, Chupeng Yang, Huodai Zhang, Jinwei Gao, Mingming Wen, Xiaosan Hu, Ziying Xu, Xin Nie and Rongwei Zhu
Submarine sinkholes are unique and important geomorphological features with a typical cavity structure that are of great scientific value. Submarine sinkholes were discovered for the first time in the isolated Ganquan carbonate platform on the Xisha Isla...
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Xiuquan Hu, Hong Liu, Xiucheng Tan, Chenjing Xiao, Qian Tan, Jianghan Li and Chi Yi
The requirements for the accurate characterization of shoal sediments have increased in view of the fact that strata are eroded due to uplift and it is difficult to calculate the real thickness of granular shoal. To solve this problem, with the shoal-to-...
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Zhen Yang, Guangxue Zhang, Songfeng Liu, Xuebin Du, Lifei Wang, Wei Yan and Lei Huang
In this study, high-resolution seismic profiles and well data provided a good opportunity for better understanding the reefs and carbonate platforms in the Wan?an Basin, southwest of the South China Sea, and also provided valuable information for the oil...
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Nicolò Del Piero, Sylvain Rigaud, Camille Peybernes, Marie-Beatrice Forel, Nicholas Farley and Rossana Martini
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Elena Liberatoscioli, Giancarlo Boscaino, Silvano Agostini, Adele Garzarella and Etta Patacca Scandone
Majella National Park is located in the central Apennines (Italy), in a vast mountainous area of about 740 km2. Owing to the complex geological history of the Majella Massif and surrounding areas, it features many different landforms. Woodlands rich in w...
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Ruth Gbadeyan and George R. Dix
The Upper Ordovician (Edenian) Lindsay Formation of the Ottawa Embayment represents the final stage of carbonate platform development in the Taconic foreland periphery inboard of the northern Appalachian orogen. The succession overlies a narrow (~60 km) ...
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Ahmer Bilal, Renchao Yang, Muhammad Saleem Mughal, Hammad Tariq Janjuhah, Muhammad Zaheer and George Kontakiotis
An integrated study based on field observation, petrography, and scanning electron microscopy (SEM) on the Early?Middle Eocene carbonate rocks has been carried out, which were deposited in the Ceno-Tethys Ocean. The study area of the Yadgaar Section lies...
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Fernando J. Gomez,Ricardo A. Astini
Pág. 19 - 46
The La Laja Formation is a key unit regarding the hypothesis of the Argentine Precordillera as a Laurentia-derived allochtonous terrane in the south central Andes. Together with the Cerro Totora Formation it comprises the oldest unit exposed at the base ...
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Elena Zoumpouli, Angelos G. Maravelis, George Iliopoulos, Chrysanthos Botziolis, Vasiliki Zygouri and Avraam Zelilidis
Field investigation, Microfacies analysis, and biostratigraphy have been carried out in the central parts of the Ionian Basin (Aetoloakarnania area, Western Greece) in order to decipher the depositional environments that developed during the accumulation...
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Manuel Martín-Martín, Francesco Guerrera, Rachid Hlila, Alí Maaté, Soufian Maaté, Mario Tramontana, Francisco Serrano, Juan Carlos Cañaveras, Francisco Javier Alcalá and Douglas Paton
An interdisciplinary study based on lithostratigraphic, biostratigraphic, petrographic and mineralogical analyses has been performed in order to establish the Cenozoic tectono-sedimentary evolution of the El Habt and Ouezzane Tectonic Units (External Int...
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Kei Ogata, ?eljko Pogacnik, Giorgio Tunis, Gian Andrea Pini, Andrea Festa and Kim Senger
The Paleogene ?megabeds? of the Julian-Slovenian Basin are regional, basin-wide deposits, produced by catastrophic carbonate platform collapses. They record the emplacement of a bipartite slide mass behaving as a cohesive blocky/debris flow in the lower ...
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Diego Alejandro Kietzmann,Verónica Vanesa Vennari
Pág. 41 - 65
The Vaca Muerta Formation in the Cerro Domuyo area shows an interesting intercalationof facies with opposite paleocurrents. The unit is represented by outer ramp to basinal facies with a westward directionof progradation. However, in its middle section, ...
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Karen Moreno,Mario Pino
Pág. 191 - 206
The characteristics of dinosaur footprints (Baños del Flaco Formation) and also the microfacies of the associated beds were analyzed. Through the footprints it was possible to interpret aspects of the dinosaur's behavior, which were very similar to the e...
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Sarah Cryer, Filipa Carvalho, Terry Wood, James Asa Strong, Peter Brown, Socratis Loucaides, Arlene Young, Richard Sanders and Claire Evans
The interface between land and sea is a key environment for biogeochemical carbon cycling, yet these dynamic environments are traditionally under sampled. Logistical limitations have historically precluded a comprehensive understanding of coastal zone pr...
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George Kontakiotis, Leonidas Moforis, Vasileios Karakitsios and Assimina Antonarakou
Sedimentological, micropalaeontological, and marine geological results from the Early Jurassic to Eocene carbonate formations of the Ionian zone, from six localities of Epirus, provide new insights into the basin palaeogeographic evolution and better cor...
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Mohammed H. N. Al-Kindi
Considering the foreland fold belt of the Salakh Arch in the northern Oman Mountains, predictions made from two-dimensional (2D) restorations and geometrical analyses are tested here to assess the relationship between large-scale folds and small-scale fr...
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Stefano Vitale, Ernesto Paolo Prinzi, Francesco D?Assisi Tramparulo, Claudio De Paola, Rosa Di Maio, Ester Piegari, Monia Sabbatino, Jacopo Natale, Pasqualino Notaro and Sabatino Ciarcia
We present a structural study on late Miocene-early Pliocene out-of-sequence thrusts affecting the southern Apennine orogenic belt. The analyzed structures are exposed in the Campania region (southern Italy). Here, thrusts bound the N-NE side of the carb...
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