The Inference of Magmatic Heat Source Beneath the Rehai (Hot Sea) Field of Tengchong From the Result of Magnetotelluric Sounding
The Inference of Magmatic Heat Source Beneath the Rehai (Hot Sea) Field of Tengchong From the Result of Magnetotelluric Sounding
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DOI：
10.1360/sb1994-39-7-572
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发表时间：
1994-04
影响因子：
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通讯作者：
白登海;廖志杰;赵国泽;王绪本
中科院分区：
文献类型：
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作者：
白登海;廖志杰;赵国泽;王绪本
1地热地质热海(热海)地热田位于北纬24°57.5‘，东经98°26.5’，海拔1400-1800米，距腾冲镇西南约18公里。热海油田具有明显的地表表现，包括沸腾的泉水和最高温度约96℃的气孔。温泉排出水为钠-氯-碳酸氢盐型，TDS为2.8g/L，SiO_2为450 mg/L。用地温计测得储集层温度一般为23o℃。这个
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_2of 450 mg/l. By geothermometers, the reservoir temperature is generally 23O℃. The