Results 81 to 90 of about 1,253 (188)

Tectonic Interplay in the Gulf of Cagliari (Italy): Extension, Compression and Strike‐Slip Movements

open access: yesBasin Research, Volume 38, Issue 3, May–June 2026.
Since the Oligocene, extensional tectonics of the Sardinia Rift and Campidano Graben interacted with the collision between Sardinia and northern Africa, generating reverse faults. At the Plio‐Quaternary boundary, compressional tectonics resumed, shaping the southern margin of the gulf through transpressional tectonics of the exposed Ichnusa High ...
Anna Del Ben   +5 more
wiley   +1 more source

The Horst of Sabzevar and regional water resources from the Bronze Age to the present day (Northeastern Iran) [PDF]

open access: yes, 2010
International audienceNumerous researchers previously explored the question of the origin of qanat system on the Iranian plateau. In 2008, the Iranian-Frenchexcavation work carried out on the site of tepe Damghani raised the issue of the evolution of ...
Julio Bendezu-Sarmiento   +10 more
core   +1 more source

Simulation of rock salt dissolution and its impact on land subsidence [PDF]

open access: yes, 2014
Extensive land subsidence can occur due to subsurface dissolution of evaporites such as halite and gypsum. This paper explores techniques to simulate the salt dissolution forming an intrastratal karst, which is embedded in a sequence of carbonates, marls,
A. Younes   +7 more
core   +1 more source

NEW ZEALAND’S TARANAKI BASIN: GIANTS IN THE GRABEN? [PDF]

open access: yes, 2002
During the past 50 years of utilising modern techniques in New Zealand’s Taranaki Basin, explorers have both been rewarded by its bountiful accumulations and frustrated by its complicated morphology.
A.W. Hart
core   +1 more source

Hydrothermal activity of the Lake Abhe geothermal field (Djibouti): Structural controls and implications for geothermal exploration

open access: yesBSGF - Earth Sciences Bulletin
This study investigates the structurally-controlled fluid flow of the Lake Abhe Geothermal Field (LAGF), using multiscale structural lineament distribution mapping and field observations. The LAGF lies within the Gob Aad graben in the Afar depression, at
Walter Bastien   +5 more
doaj   +1 more source

Land use in the tropical karst - the case of Peruaçu, Januària and Jaiba; SE Brazil. [PDF]

open access: yesInternational Journal of Speleology, 1999
The karstic regions of the municipalities of Peruaçu, Januària and Jaiba present a variety of soil uses which are a function of the organization of the karstic relief.
Kohler Heinz Charles   +2 more
doaj  

Tectónica de fracturas en el suroeste de colombia [PDF]

open access: yes, 1986
En algún tiempo se pudo pensar que en la tectónica de los Andes de Colombia tenían muchísima importancia los pliegues y muy poca las fallas y, en gran escala, las fracturas mayores.
Acosta A., Carlos E.
core  

Extensional Tectonic Regime of Garut Basin based on Magnetotelluric Analysis

open access: yesIndonesian Journal on Geoscience, 2014
DOI: 10.17014/ijog.v8i3.162Garut Basin are is part of Bandung-Garut Greater Basin (Bandung Zone) characterized by a large basin surrounded by mountain ranges. Active volcanoes had distributed their material as pyroclastic deposits around the outer border
Lina Handayani   +2 more
doaj   +1 more source

Seismic interpretation for the Jurassic/Paleozoic reservoirs of QASR gas field, Shushan-Matrouh basin north Western Desert, Egypt

open access: yesEgyptian Journal of Petroleum, 2019
The QASR gas field lies in the northern part of Shushan-Matrouh Basin (northern part of the Western Desert). Jurassic (Lower Safa)/Paleozoic are a reservoir rocks, in which the gas is trapped in clastic Sandstone, depending on structural framework ...
Mohammed Abuzaied   +4 more
doaj   +1 more source

An Integrated Surface and Borehole Seismic Case Study: Fort St. John Graben Area, Alberta, Canada [PDF]

open access: yes, 1993
The deltaic sandstones of the basal Kiskatinaw Formation (Stoddard Group, upper Mississippian) were preferentially deposited within structural lows in a regime characterized by faulting and structural subsidence. In the Fort St.
Richards, Barry R.   +3 more
core   +2 more sources

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