Results 51 to 60 of about 276 (181)
Abstract In the northwestern Gulf of Mexico, gravity‐driven contractional deformation is recorded across the Salina del Bravo, the Perdido and Peripheral fold belts, and the Mexican Cordilleras. Integrating seismic interpretation, structural mapping, and analysis, we examine the spatial and temporal partitioning of shortening above three principal ...
F. A. Rodriguez‐Roa +2 more
wiley +1 more source
Structural evaluation and hydrocarbon potentials of Emil Field, offshore Niger Delta Basin
The Emil Field, located in the deep offshore Niger Delta Basin, represents a structurally complex petroleum system shaped by sediment loading, growth faulting, and shale diapirism. This study applies an integrated workflow of seismic interpretation, well
Ekwu Victor Chukwuemeka +3 more
doaj +1 more source
Formation and growth of diapirs in contractional settings: the Mediano anticline and Clamosa diapir case study (Southern Pyrenees) [PDF]
At the northwestern termination of the South Pyrenean Central Salient, thrust imbrication, detachment folding and diapirism are structurally and genetically related. The La Fueba imbricate system has been folded by the Mediano detachment anticline, while
P. Santolaria +5 more
doaj +1 more source
Timing of the Albano‐Hellenic Paleomagnetic Rotation
Abstract The Aegean arc is the most prominent Mediterranean salient, characterized by significant paleomagnetic rotations along its limbs. Although it is well‐established that the external Ionian and Kruja zones of the Albano‐Hellenides underwent a ∼40° post‐Oligocene clockwise (CW) rotation relative to Africa/Adria, the rotation timing remains debated.
F. Feriozzi +4 more
wiley +1 more source
Causes of Multi-Mechanism Abnormal Formation Pressure in Offshore Oil and Gas Wells
This study thoroughly investigates the complex origins of abnormal formation pressure in offshore oil and gas wells, taking the Rio del Rey Basin in Cameroon as a case study.
Yang Xu +5 more
doaj +1 more source
Evidence for the origin of ridges on Europa by means of photoclinometric data from E4 Galileo orbit [PDF]
The most commonly observable structures on the surface of the Jovian satellite Europa are the ridges. Geological evidences show that the ridges have been formed continuously for the last 10 million years.
Blanca Mendoza, Guadalupe Cordero
doaj
Abstract Deep fluid advection fundamentally governs the thermal‐fluid‐chemical evolution and distribution of hydrate‐cold seep systems. However, coupled relationships between deep fluid and shallow multiphase dynamics remain inadequately constrained.
Wei Huang +6 more
wiley +1 more source
Troodos: A Giant Serpentinite Diapir
Troodos is a classical ophiolite complex. It is proposed that the serpentinized harzburgites that now form the top of the mountain and represent the originally lowest part of the ophiolite sequence rose as a diapir. This diapiric rise is caused by the pervasive serpentinization of a suboceanic harzburgite, due to rock-sea water interaction.
openaire +3 more sources
Abstract Salt tectonics has received little attention in the Middle Atlas, despite the widespread occurrence of Triassic evaporites and their potential to exert first‐order control on basin architecture and deformation. This study presents the first integrated analysis of polyphase salt tectonics in the Middle Atlas, focusing on the Oum Er‐Rbia sector,
N. Saspiturry +10 more
wiley +1 more source
Geoarchaeological Evidence for the Decline of the Medieval City of Qalhat, Oman
The medieval city of Qalhat was an important trade town along the sea routes in the Indian Ocean. The reasons for the decline of the city are unclear, as the archaeological evidence is inconclusive.
Alina Marie Ermertz +4 more
doaj +1 more source

