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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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José Duque-Trujillo,Camilo Bustamante,Luigi Solari,Álvaro Gómez-Mafla,Gloria Toro-Villegas,Susana Hoyos
Pág. 82 - 101
The Antioquia batholith represents the magmatic record of the interaction between the Farallón and Caribbean plates with the NW part of the South American Plate during the Meso-Cenozoic. Several authors have reported zircon U-Pb ages and whole rock geoch...
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Cuiying Zhou, Xu Yang, Yanhao Liang, Zichun Du, Zhen Liu, Wei Huang and Weihua Ming
Red beds are Meso?Cenozoic continental sedimentary strata that are mainly composed of gravel stone, sandstone, siltstone, mudstone, and shale and occasionally have interlayers of limestone, halite, and gypsum. As a typical rock mass, red beds are widely ...
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Constantino Mpodozis
RESUMEN:Las Islas Ildefonso, ubicadas en la shelf magallanica al sur de Isla Hoste, estan constituidas por una secuencia sedimentaria de 100 m de espesor, donde se reconoce una sucesion de facies de turbiditas proximales, turbiditas distales y conglomera...
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Xu Lin, Marc Jolivet, Jing Liu-Zeng, Feng Cheng, Zhonghai Wu, Yuntao Tian, Lingling Li and Jixin Chen
Understanding the formation of the North Qilian Shan in the NE Tibetan Plateau provides insights into the growth mechanisms of the northern region of the plateau across time. Detrital zircon fission-track (ZFT) analyses of river sediments can provide a c...
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Stefano Vitale, Ernesto Paolo Prinzi, Maria Monda, Francesco D?Assisi Tramparulo and Sabatino Ciarcia
We present a structural study on the tectonic windows of Giffoni and Campagna, located in the western sector of the southern Apennines (Italy). We analyzed thrusts, folds, and related minor deformation structures. Here, a major in-sequence E-verging thru...
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