Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia)

Новиков, Д. А.

doi:10.1007/s12517-016-2792-0

Cited by 9 publications

(3 citation statements)

References 17 publications

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“…4. Hydrogeochemical and hydrodynamic search and evaluation criteria have been developed for oil, gas and ore deposits and are used to evaluate prospects and explain concepts of development of deposits in the Siberian region [19][20][21].…”

Section: Resultsmentioning

confidence: 99%

The HydroGeo Software Package and Its Usage

2019

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Section: Resultsmentioning

confidence: 99%

The HydroGeo Software Package and Its Usage

2019

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“…The new geothermal data, along with the results of the studies mentioned previously (Novikov and Shvartsev, 2009;Dultsev and Novikov, 2017;Novikov, 2017a;Novikov et al, 2018), allowed us to revise the key geothermal features of the subsurface of the region under study, enabling the development of the first geothermal model of this area.…”

Section: Methodsmentioning

confidence: 93%

Geothermal Model of the Fore‐Yenisey Sedimentary Basin—Transitional Structure between the Ancient Siberian Platform and the Young West Siberian Plate

Novikov

Dultsev

Filippov

2022

Acta Geologica Sinica (Eng)

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Results of the investigation into the geothermal regime of the Fore‐Yenisey sedimentary basin, formed during the collision and subsidence of the Kas‐Turukhan microcontinent and the western margin of the Siberian craton in the late Neoproterozoic and early Paleozoic are reported. It was established that the structural and geothermal conditions of the upper Precambrian–Paleozoic sections are similar to those in the western regions of the Siberian platform and are characterized by rather low geothermal gradients (12.5–25.5 °C/km). In the western parts of the basin, formation temperatures in the uppermost pre‐Jurassic sediments are 50°C–85°C, decreasing eastward to 30°C–55°C. For the first time, the detailed geothermal model of the basin sedimentary fill was developed. This model allows predictions of the geothermal conditions of Earth's interior.

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“…In accordance with hydrogeological zoning, Yurubcheno-Tokhomskaya area is situated within second-order Kamo-Vel'minskii Artesian Basin in the southwestern part of Tungusskii Artesian Basin, East-Siberian Artesian Province [1]. [2][3][4], have been carrying out the study of the chemical analysis of groundwater and brines of the Tunguska artesian basin.…”

Section: Introductionmentioning

confidence: 99%

Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone

Trifonov

2019

E3S Web Conf.

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In this study the chemical analysis of groundwater in Yurubcheno-Tokhomo hydrocarbon accumulation zone (YTHAZ) was carried out. The analysis revealed that fresh, brackish, saline waters and brines of various chemical types occur in the study area. Water salinity increases with the depth, but this dependency is not observed in Vendian and Riphean oil and gas deposits. The most mineralized brines occur in the salt-bearing hydrogeological formation. On the basis of the data on the geochemistry of groundwater, the possibilities of their further practical application were determined.

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Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia)

Cited by 9 publications

References 17 publications

The HydroGeo Software Package and Its Usage

The HydroGeo Software Package and Its Usage

Geothermal Model of the Fore‐Yenisey Sedimentary Basin—Transitional Structure between the Ancient Siberian Platform and the Young West Siberian Plate

Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone

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