Estilos geotectónicos bidimensionales y tridimensionales interbloques: Una nueva categoría neotectónica para la determinación de morfoestructuras montañosas [PDF]
Investigaciones Geográficas, 1994 Cuban Archipelago geologic evolution reveals a W to E migration in Early Mezo–Cenozoic vulcanism and magmatism as well as an increased activity in neotectonics, seismicity, and recent secular endodynamics originating a conspicuous geomorphological ...
José Ramón Hernández Santana +2 more
doaj +4 more sources
Geología, evolución estructural (Eoceno al actual) y eventos sísmicos del Graben de Santiaguillo, Durango, México [PDF]
Revista Mexicana de Ciencias Geológicas, 2014 El graben de Santiaguillo forma la parte noroccidental del sistema regional de fallas San Luis-Tepehuanes, y se encuentra ubicado entre las provincias de la Sierra Madre Occidental y de la Mesa Central.
Angel Francisco Nieto-Samaniego +5 more
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Study of the sub-surface geological condition of the Sibalaya flow liquefaction using seismic refraction method [PDF]
E3S Web of Conferences, 2023 Understanding the occurrence of flow liquefaction requires knowledge of the sub-surface condition controlling its occurrence. This paper presents the results of seismic refraction surveys conducted to evaluate the sub-surface geological condition in the ...
Pradnya Andika Putu +2 more
doaj +1 more source
Extension and inversion of salt-bearing rift systems [PDF]
Solid Earth, 2020 We used physical models to investigate the structural evolution of segmented extensional rifts containing syn-rift evaporites and their subsequent inversion. An early stage of extension generated structural topography consisting of a series of en-échelon
T. P. Dooley, M. R. Hudec
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Morphotectonic Evolution of Selduk Graben in Development Process of Western Anatolian Grabens [PDF]
, 2023 Gurer, Omer Feyzi/0000-0001-7210-769XThe Selduk Graben is the name given to the young graben developed in the western tip of the Kuduk Menderes graben. It was a part of the main graben until a strike-slip fault zone cut and displaced it to the southwest ...
Erbay, Yucel +2 more
core +1 more source
, 2016 Ensino Médio::GeografiaThe animation shows the formation of horst and graben, geomorphologic features caused by the movement of the earth’s crust. The horst is generated when two regions suffer compression and a part of the crust is upthrown, while the ...
U.S. Geological Survey
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The first result of geodetic implications on intra-graben subsidence along the eastern part of the Gediz graben [PDF]
, 2021 The Western Anatolian extensional tectonic regime results in developing a set of approximately E-W trending Horst-Graben morphology. The Gediz graben accommodating many fertile lands is one of the significant tectonic structures associated with that ...
Hastaoğlu, Kemal Özgür +7 more
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From shallow-water carbonate ramp to hemipelagic deep-marine carbonate deposition: Part 1. General characteristics, microfacies and depositional history of the Middle to Late Anisian Bulog sedimentary succession in the Inner Dinarides (SW Serbia) [PDF]
Geološki Anali Balkanskoga Poluostrva, 2023 The opening of the Neo‐Tethys started in the Middle Anisian and is recorded in the drowning succession of the shallow‐water Ravni/Steinalm Carbonate Ramp and the subsequent deposition of deep‐marine limestones, e.g., the red nodular limestones of the ...
Gawlick Hans-Jürgen +5 more
doaj +1 more source
, 2011 A animação mostra a formação do horst e do graben, feições geomorfológicas causadas pela movimentação da crosta terrestre. O horst é gerado quando duas regiões sofrem compressão e uma parcela da crosta terrestre é soerguida, enquanto o graben ocorre ...
U.S. Geological Survey
core +4 more sources
Frontiers in Earth Science, 2022 The island of Ischia, an active volcanic field emerging in the western sector of the Gulf of Naples (Southern Italy), represents an archetypal case of caldera that underwent a very large resurgence related to the intrusion of a shallow magma body.
Stefano Carlino +7 more
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