New data on the temperature regime of the Udachnaya kimberlite pipe (YASSR)
Authors:
Abstract
The Udachnaya kimberlite pipe is located on the southern slope of the Anabar anteclise. The sedimentary section intervening the pipe is represented by carbonate (calcareous-dolomitic) sediments of the Cambrian and Upper Proterozoic with a thickness of up to 4000 m.
Область исследования:
(Archived) Without section
References
- Klimovsky I.V., Ustinova Z.G. On the peculiarities of the temperature regime of perennially frozen rocks in the area of the kimberlite pipe Udachnaya. PH of the AS USSR, 1962.
- Makarov K. K. Structure of the crystalline basement on the southern slope of the Anabar anteclise in connection with the assessment of oil and gas bearing prospects. - Proc. VNIGRI, issue 249, 1966.
- Melnikov P. I. Influence of Groundwater on Deep Cooling of the Upper Zone of the Earth Crust. Nauka, 1967.
- Neizvestnov Ya. V., Tolstikhin N. I. Negative-temperature waters of the Arctic and Subarctic - cryopegs and their significance in the transport of chemical substances. Theses of reports to the conference “Geochemical Prospecting in the Regions of Cryogenesis”. PH of the Research Institute of Arctic Geology, 1970.
- Slavin V.I. About hydrogeological conditions of the Markhinskaya reference well area on the southern slope of the Anabar anteclise. - Proc. VNIGRI, vol. 240, 1966.
- Slavin V. I, Grubov L. A. Hydrogeologic features of the Markhinsky Shaft in connection with the assessment of its prospects for oil and gas. Nedra, 1968.
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