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The Inference of Magmatic Heat Source Beneath the Rehai (Hot Sea) Field of Tengchong From the Result of Magnetotelluric Sounding 被引量:20

The Inference of Magmatic Heat Source Beneath the Rehai (Hot Sea) Field of Tengchong From the Result of Magnetotelluric Sounding
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摘要 1 Geothermal Geology The Rehai (Hot Sea) geothermal field is at 24°57.5′N and 98°26.5′E in amountainous (1400-1800 m) area, approximately 18 km southwest of TengchongTown. The Rehai field has noticeable surface manifestations including boiling springsand fumaroles with a maximum temperature of about 96℃. The thermal springsdischarge water of the sodium-chloride-bicarbonate type with TDS of 2. 8 g/l and SiO<sub>2</sub>of 450 mg/l. By geothermometers, the reservoir temperature is generally 23O℃.
出处 《Chinese Science Bulletin》 SCIE EI CAS 1994年第7期572-577,共6页
基金 The project of "Eighth Five" scientific and technological research of the State Science and Technology Commission of China.
关键词 geothermal FIELD MAGMATIC heat source MAGNETOTELLURIC sounding. GEOTHERMAL FIELD MAGMATIC HEAT SOURCE MAGNETOTELLURIC SOUNDING
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