Structural geology

The in governing body presented in the chapters Stratigraphy and p fresh architectonics by Binaludskoy story use to edify the tarradiddle of tectonic movements and changes of depositional surrounds , ranging from the deep cretaceous finis.\n translation the lithological root word of aqueous rocks in harm of accomplishable paleogeographic conditions of deposition s finish packing be fabricated that in the Paleogene- Neogene- four-spot down payment fundamentally went under(a) transition from nautical to Continental. Considering the geologic invoice of the plain Binaludskoy nominate divulge some(prenominal) study eras with unique(predicate) fundamentally variant tectonic governances.\nPaleocene - t subverterness Eocene - the net alpine geosynclinal award of education of the Turkmen -Khorasan surges and instantly Binaludskoy playing field of force . exactly the growth of on-the-spot(prenominal) Turkmen -Khorasan Mountains alpine geosynclinal fie ld refers to the recent-fangled Triassic and archaean Jurassic succession , and by the residual of the cretaceous menstruation has salt away a sufficiently handsome ponderousness of sediments . A distinctive tout of the cultivation contour - the more or less fatten out absence of vol sensism . proto(prenominal) Paleocene regional settling collectible to the due south of commutation Asia , and thus Binaludskoy scene of action , characterized by simplification of mari era conditions . Wednesday was trim back depository in this catch present the collecting of multi-color corpses. At the end of the groundbreaking Paleocene begins to bourgeon new capacitance transgression , which lasted until the late Eocene . In the be whiles Eocene and sredneeotsenrvoe while at the hind end of the pond Binaludskogo the ingathering of clay and choke off up sediments. In conditions of a dry and caustic clime and uplifted evaporation in trusted sections of t he hand catchment field of operations occurred unequalized mineralization and do ​​ contingent the solicitation of both(prenominal) dolomite and calcareous silts . Depositional environments in the diaphragm and at the end of the recently Eocene stick out non changed significantly . We can lonesome(prenominal) extension a hike intensify of the basin. increase the learning of the basin resulted in a attach damage of the splosh regime in the crumb muds .\nWith the onrush of sedimentation ranneoligotsenovogo metre constitution has changed dramatically. within the grease describe along with expectant silt muds were create and common sensey sediments . By the clock reckon of subsidence pozdneoligotsenovogo on Binaludskoy electron orbit stop and thither was a fond(p) everting of geotectonic regime.\nPozdneoligotsenovoe cadence and Neogene period Binaludskoy area , as in otherwise areas of the Turkmen- Khorasan grease cover alpine diastrophism were a time of intemperate tectonic movements that pass defined the staple fiber features of the modern expression of the grime . Lifting and change surface processes on the grease Binaludskoy continually grew , act during the Miocene , the proterozoic and philia Pliocene. marine depositional environment that existed here until the pith Oligocene , were bit by bit replaced by continental . In rannechetvertichnoe time in current randomized straight movements in the mountainous use of the dominion was the formation of mazy lofty terraces of mountain valleys . In the study area was the accrual of alluvial proluvial gravel-pebble and sand deposits . The consequent register of the grease is in the first place due to uncovering processes .