scholarly journals Downhole Temperature Measurements and Heat Flow Data in the Black Sea—DSDP Leg42B

1978 ◽  
Author(s):  
A.J. Erickson ◽  
R.P. Von Herzen
Keyword(s):  
Heat Flow ◽  
Black Sea ◽  
Temperature Measurements ◽  
The Black Sea ◽  
Flow Data ◽  
Downhole Temperature

Thermal structure of the crust in the Black Sea: comparative analysis of magnetic and heat flow data

2014 ◽  
Vol 35 (4) ◽  
pp. 345-359 ◽  
Author(s):  
V. I. Starostenko ◽  
M. N. Dolmaz ◽  
R. I. Kutas ◽  
O. M. Rusakov ◽  
E. Oksum ◽  
...  
Keyword(s):  
Comparative Analysis ◽  
Heat Flow ◽  
Black Sea ◽  
Thermal Structure ◽  
The Black Sea ◽  
Flow Data

Age, thermal evolution and history of the Black Sea Basin based on heat flow and multichannel reflection data

1992 ◽  
Vol 210 (3-4) ◽  
pp. 273-293 ◽  
Author(s):  
A.Ya Golmshtok ◽  
L.P Zonenshain ◽  
A.A Terekhov ◽  
R.V Shainurov
Keyword(s):  
Heat Flow ◽  
Black Sea ◽  
Thermal Evolution ◽  
The Black Sea ◽  
Reflection Data ◽  
History Of

scholarly journals Heat flow investigations in the Narssaq and Ivigtut areas

1971 ◽  
Vol 35 ◽  
pp. 25-27
Author(s):  
B.L Nielsen
Keyword(s):  
Heat Flow ◽  
World Wide ◽  
Flow Patterns ◽  
Temperature Measurements ◽  
Flow Data ◽  
Flow Investigation ◽  
Drill Holes

Temperature measurements in drill holes have been carried out in the Ivigtut area and in the Ilimaussaq intrusion near Narssaq as the start of a general heat flow investigation in South Greenland. As this kind of work has not previously been done in Greenland and heat flow data from arctic areas are still very few it is hoped that the results will contribute to a better understanding of world-wide heat flow patterns and their relationship to major tectonic provinces.

Heat flow and geothermal model of the Black Sea depression

1998 ◽  
Vol 291 (1-4) ◽  
pp. 91-100 ◽  
Author(s):  
R.I. Kutas ◽  
V.P. Kobolev ◽  
V.A. Tsvyashchenko
Keyword(s):  
Heat Flow ◽  
Black Sea ◽  
The Black Sea ◽  
Geothermal Model

Heat flow and thermal evolution of the lithosphere of the Black Sea basin

Oceanology ◽  
2006 ◽  
Vol 46 (2) ◽  
pp. 274-291 ◽  
Author(s):  
Yu. I. Galushkin ◽  
A. A. Shreider ◽  
A. A. Bulychev ◽  
Al. A. Shreider
Keyword(s):  
Heat Flow ◽  
Black Sea ◽  
Thermal Evolution ◽  
The Black Sea

scholarly journals Geothermal field of the transition area between the Anatolian Plate and the East European Platform

2019 ◽  
pp. 133-148
Author(s):  
Mansouri Far Siamak
Keyword(s):  
Heat Flow ◽  
Black Sea ◽  
Eastern Mediterranean ◽  
Eastern Mediterranean Region ◽  
The Black Sea ◽  
Flow Density ◽  
Heat Flow Density ◽  
Western Turkey ◽  
East European ◽  
East Anatolia

Heat flow data from the Eastern Mediterranean region indicates an extensive province of low heat flow, spreading over the whole basin of the Mediterranean to the east of Crete (Levantine Sea), Cyprus, and Northern Egypt. Surface geology of East Anatolia is complex because of recent active tectonic and volcanic activity. The region is composed of major tectonic units of Pontides, the Anatolid-Tauride Belt and Bitlis Suture Zone, North and East Anatolian faults. Ophiolitic and young volcanic rocks can be observed in many parts of East Anatolia. The Black Sea is surrounded by the Alpine-Himalayan Orogenic Belt of Crimea, Greater Caucasus, Pontides, Rhodope-Stranja Massif, Eastern Srednegorie, North Dobrogea and older tectonic units of different origins and ages such as the Precambrian East European Craton, Moesian Platform, Istanbul Zone and Adzhar-Trialet Folded System. Low heat flow density dominates in the Black Sea. The lowest (less•30 mW/m2 ) values have been recorded in central parts of the Western and Eastern Black Sea basins with maximal sedimentary thickness. Geothermal studies within the territories of Ukraine have been under way since sixties. Many important features of the thermal field remain unstudied. This applies in particular to the Ukrainian Shield and to the southern part of the Carpathian region. In general, the territory of Alpine folding within Turkey, Marmara and Aegean seas, Caucasus is characterized by high heat flow. The anomaly of its highest values (above 100 –150 mW/m2 ) exists within western Turkey, where tectonic conditions of extension prevail and underground steam is used to produce electricity. Three heat flow density profiles crossing the studied region and heat flow map were compiled.

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