The formation features of landscapes in the Inderskii salt-dome area (Precaspian Hollow)

Petrishchev, V. P.; Чибилев, А. А.; Ахмеденов, К. М.; Ramazanov, S. K.

doi:10.1134/s1875372811020077

Cited by 6 publications

(5 citation statements)

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“…S. S. Korobov and I. K. Polenov [6] single out a number of factors, that contribute to karst development over the Inder uplift:…”

Section: Resultsmentioning

confidence: 99%

“…Formation of secondary (karst-tectogenic) cap rock is associated with the wet postglacial epochs, and also with the leaching by sea water during the Caspian transgressions periods. The cap rock formation process led to the formation of various minerals, including unique: vitchite, gergeyite, hydroboracite, inderborite, inyoite, colemanite, kurnakovite, sulphoborite [6].…”

Section: Resultsmentioning

confidence: 99%

“…Inder dome cap rock is surrounded by fractured-karstic suprasalt waters. Inder cap rock has an extremely high filtration capacity: 300 -500 l/day [6]. Aquifer recharge is performed by atmospheric precipitation and transit streams directed towards Inder Lake.…”

Section: Resultsmentioning

confidence: 99%

“…Schematic map of karstic phenomena and processes expansion over the West Kazakhstan territory was drawn up on the basis of various literary sources [3][4][5][6], where there were descriptions of karstic relief effects within the region, and also descriptions of scientific expedition results in 2012 on the territory of Burlin and Syrym regions of WK. For making the hypsometric basis for this map there were used public data of satellite radar topographic mapping (SRTM) processed in ArcGIS 9.2.…”

Section: Methodsmentioning

confidence: 99%

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Karst and Pseudokarst of the West Kazakhstan (Republic of Kazakhstan)

Ахмеденов¹,

Iskaliev²,

Petrishev³

2014

IJG

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An analysis of the formation of karst and karst-suffosion forms on the territory of the West Kazakhstan region is presented in this paper. Numerous literary sources were used as the information database for the analysis of the relief features of the West Kazakhstan region. Evaluation of the morphometric features of the collapsed new formations on the basis of materials of our own field research is presented here for the first time. According to the research objectives there were defined localization places of the karst-collapsed phenomena where the reconnaissance field surveys were carried out. Survey points' localization has been carried out by means of GPS system with the help of 12-channel GPS-receiver of Garmin eTrex model. Geoinformational technology, based on MapInfo 9.5 and ArcGIS 9.2 packages was used for the building of the information and cartographic database. Original thematic maps compiled on the basis of the research results' analysis have been obtained in this research. The features of the Caspian Basin's karst landscapes, formed as a result of salt-dome tectonic manifestations (Inder Mountains, Malaya Bogdo Mountain, Bish-Chokho hill) are described in this paper. The important elements of the Caspian Basin salt-dome landscapes are landforms of the karst origin from large karst depressions of the karst-tectonic origin to modern forms of the sulfate karst: sinkholes, wells, polje, knobs ("Kurgantau"), arches, caves and grottoes. Some karst formations have a non-salt-dome origin. Three areas with the collapsed forms that have the karst-suffosion origin have been identified (near Konyr village, Berezovka village and Zhanatalap village). The mechanism of the sinkholes formation is due to the changes of the groundwater regime and the displacement of limestone eluvium as a result of active anthropogenic impacts. The sinkholes occurence near Zhanatalap village, which is located near the Karachaganak oil and gas field, is probably due to the anthropogenic initiation of karst-suffosion processes.

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“…S. S. Korobov and I. K. Polenov [6] single out a number of factors, that contribute to karst development over the Inder uplift:…”

Section: Resultsmentioning

confidence: 99%

Section: Resultsmentioning

confidence: 99%

Section: Resultsmentioning

confidence: 99%

Section: Methodsmentioning

confidence: 99%

See 2 more Smart Citations

Karst and Pseudokarst of the West Kazakhstan (Republic of Kazakhstan)

Ахмеденов¹,

Iskaliev²,

Petrishev³

2014

IJG

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“…That is when these parameters are larger than an order of magnitude compared to the subgrade structure size, the roadbed will be destabilized. And when these parameters are smaller than an order of magnitude compared to the subgrade structure size, the effects could be negligible [6]. When there is not much karst under the roadbed, its roof is thicker and the rock is hard and complete, which does not affect driving safety, it is generally not handled.…”

Section: The Scale Effect Of Karst Formmentioning

confidence: 99%

Discussion on Damages of Karst to Roadbed and Its Countermeasures

Wang¹

2018

OJCE

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Because of the long-term dissolution of water, the formation of karst caves and fissures in rock formations are called karst. In Karst area, deformation and water damage are the main forms of karst damage to subgrade. Uneven settlement of embankment and instability of subgrade are the concrete manifestations of karst roadbed diseases. Therefore, considering the scale effect of karst, the concrete treatment measures of karst roadbed should be put forward and the principle of prevention and treatment of "dredging, crossing, reinforcing and blocking" should be followed, based on the characteristics of various karst forms, such as section funnel, depression, karst cave, solution crack and karst spring.

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The landscape and biological diversity of salt-dome landscapes: specific features (Western Kazakhstan case study)

Ахмеденов

2018

Arab J Geosci

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The formation features of landscapes in the Inderskii salt-dome area (Precaspian Hollow)

Cited by 6 publications

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Karst and Pseudokarst of the West Kazakhstan (Republic of Kazakhstan)

Karst and Pseudokarst of the West Kazakhstan (Republic of Kazakhstan)

Discussion on Damages of Karst to Roadbed and Its Countermeasures

The landscape and biological diversity of salt-dome landscapes: specific features (Western Kazakhstan case study)

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