Information om | Engelska ordet ANTICLINAL

Exempel på hur man kan använda ANTICLINAL i en mening

• Colerain valley (shown as "Friends Cove" on topographic maps) is an anticlinal valley, with Evitts Mountain and Tussey Mountain forming the limbs.
• The Vindhyas do not form a single range in the proper geological sense: the hills collectively known as the Vindhyas do not lie along an anticlinal or synclinal ridge.
• The Burgan field's structure is an anticlinal dome having an elliptical shape and transected by numerous radial faults.
• These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations.
• The development of the aleurone layer involves several periclinal, and anticlinal cell divisions and several steps of genetic regulation.
• Nittany Mountain is part of a synclinal depression of the anticlinal Nittany Arch, which originally formed a huge mountain, since eroded, that towered over what is now Nittany Valley.
• The field is an anticlinal structure on the downthrown side of a major salt diapir associated growth fault and produces from 25 Pliocene-Pleistocene delta-front sandstone reservoirs at depths from 1290 to 3600 m.
• The 'Simply Folded Belt' of the Zagros Mountains – A series of elongated anticlinal domes, mostly formed as detachment folds over underlying thrusts in the foreland of the Zagros collisional belt, generally above a basal decollement that formed in evaporite of the late Neoproterozoic to Early Cambrian Hormuz Formation.
• The trap is mainly anticlinal 4-way rollover but internally the doubly plunging anticline is cored by a small reverse fault and upwardly diapiric mobile shale or mud.
• The North Belridge Field, like the South Belridge and the others nearby (Cymric, Monument Junction, McKittrick, Antelope Hills, and others) is near the western margin of the huge San Joaquin Basin, a region of extensive sedimentary rocks of varying porosity and permeability, containing anticlinal folds and copious quantities of petroleum, much of which has been extracted in the early and middle 20th century.
• In 1901 the Orcutt field was discovered, and in 1903 the discovery well for the Lompoc field was drilled, after several failed attempts to find oil in the obviously promising anticlinal structure.
• The Oklahoma City Oil Field is in a faulted anticlinal structure located on the southern end of the Nemaha Ridge and the northeast rim of the Anadarko Basin.
• Along with the Dos Cuadras field to the west, the Carpinteria offshore field is part of a larger anticlinal trend beginning on land north of Ventura with the Ventura Oil Field, and continuing with breaks west through the San Miguelito and Rincon oil fields, then running offshore to the Carpinteria and Dos Cuadras fields underneath the Santa Barbara Channel.
• Continued shortening and excess material within the anticlinal core not only results in increased amplitude and disharmonic folds, but may lead to the onset of thrusts out of the folded synclinal or anticlinal regions.
• Their cuticle tissue is a palisadoderm, comprising parallel or roughly parallel hypha arranged in an anticlinal fashion.
• The rock of Siletzia has been exposed in various places by tectonic uplift (as around the periphery of the Olympic Mountains), anticlinal folding (such as the Black Hills and Willapa Hills in southwestern Washington), and overthrusting onto other formations (along various faults in central and southern Oregon).
• It is the central portion of the Olympic–Wallowa Lineament, referred to as the Cle Elum-Wallula deformed zone (CLEW), constising of a series of generally east-trending narrow asymmetrical anticlinal ridges and broad synclinal valleys formed by folding of Miocene Columbia River basalt flows and sediments.
• In the Eastern Asian Mesozoic Folding Zone, Eastern part of the Khingan-Okhotsky Volcanic Belt, at the intersection of the major Sikhote Alin - Mongol-Okhotsk tectonic systems and within the western part of the Sikhote Alin geanticlinal and silicate system, coinciding with the NE junction of the Badzhalsky anticlinal lifting with the Gorin downfold Left shore of the Amur, in the basins of the Silinki and Gorin tributaries.
• The synclinals of the Río Frío, Checua-Lenguazaque, Sesquilé, Sisga, Subachoque, Teusacá, Siecha, and the anticlinal of Guatavita are composed of the Cacho Formation.
• Composed primarily of Mesozoic and Paleogene limestones, Nemërçka features a heavily karstified ridge, formed by an elongated anticlinal structure, embanking the graben valley of Vjosë.

Förberedelsen av sidan tog: 381,00 ms.