References
This section lists all references that have been added to this portal. You can search and filter references by type, author, title, and other metadata. Each reference may include a DOI, publication date, and other relevant information to help you find and cite the literature effectively.
Thermal Regime of the State 2–14 Well, Salton Sea Scientific Drilling Project
Temperature logs were made repeatedly during breaks in drilling and both during and after flow tests in the Salton Sea Scientific Drilling Project well (State 2–14). The purpose of these logs was to assist in identifying zones of fluid loss or grain and to characterize reservoir temperatures. At the conclusion of the active phase of the project, a series of logs was begun in an attempt to establish the equilibrium temperature profile. Initially, we were able to log to depths below 3 km, but beginning in late May of 1986, it was impossible to log below about 1.8 km owing …
Geotermicheskie Is-Issledovanija Barsukovskogo Neftjanogo Mestorozhdenija (PripjatskijProgib) (Geothermal Survey of the Barsukovskoe Oil Field (PripyatskiiProgib) )
Geothermal studies in the Quemado area, New Mexico
New heat-flow data and K-Ar dates from the southern periphery of the Colorado Plateau (CP) are presented. The radiometric data indicate the area around Quemado, NM was volcanically active during mid- and late-Pliocene time. The heat-flow data suggest a regional value for the area of 75–84 mW m−2, somewhat higher than the non-volcanic regions of the Plateau. The average heat flow in the Quemado area is 10–20 mW m−2 less than the heat flow in the north-western periphery of the Plateau where a transition zone between the Basin and Range Province (BRP) and the CP is present. From geophysical data …
Terrestrial heat flow above the Andean Subduction Zone in Bolivia and Peru
Teplovoj potok Baltijskoj SineklizyI Nekotorye Aspekty Ego Svjazi S Glubinnym Stroeniem Zemnoj Kori (Heat flow of the Baltic Syneclise, Some Aspects of Its Relationship with the Deep Structure of the Earth's Core )
The distribution of geothermal and geochemical gradients near site 501/504: Implications for hydrothermal circulation in the oceanic crust
Significance of past and recent heat-flow and radioactivity studies in the southern Rocky Mountains region
Deep structure of the Hoggar domal uplift (Central Sahara, south Algeria) from gravity, thermal and petrological data
Atlas of geothermal resources in the European Community, Austria and Switzerland
New heat flow investigations in Arkansas
Geophysical survey of a mud volcano seaward of the Barbados ridge accretionary complex
Conductive heat flux in VC-1 and the thermal regime of Valles Caldera, Jemez Mountains, New Mexico
pers. comm
Temperature, thermal conductivity, and heat flow near Yucca Mountain, Nevada: Some tectonics and hydrologic implications
Study on the geothermal field in North China
Subduction of the Juan de Fuca Plate: Thermal consequences
Thermal evolution of the western Svalbard margin
Scientific Cruise Report of Arctic Expedition ARK IV/3
Yavorovskaya anomaliya teplovogo potoka - geofizicheskii zhurnal 1988 (Yavorovska Heat Flow Anomaly )
Characteristics of geothermal field in Yunnan region
This paper provides 14 values of-geothermal heat flow obtaind from the geothermal measurement of 26 wells. Based on these data the characteristics of the geothermal field in Yunnan region have been described as follows: Either the distribution of geothermal heat flow, or the variation of temperature gradient displays high value in the west of Lancangjiang river, the northern segment of Honghe fault zone, as well as Kunming and Eshan region. Low value occurs to the east of Xiaojiang fault zone in eastern Yunnan, and also in the region between the Xiaojiang and Honghe fault zones, including Chuxiong, Binchuan and Xiangyun. …