1) origin of geoheat
地热成因
1.
From the viewpoint of the origin of geoheat of Tengchong,the overall hydrochemical characteristics and mode of occurrence of the geothermal water there are analyzed.
本文从腾冲地热成因的角度，分析其地热水化学的总体特征和赋存规律。
2) origin of geothermal field
地热田成因
1.
The paper introduces a geologic model of origin of geothermal field by studying low-medium temperature geothermal system of convective type of geothermal field in south of Chifeng-Chaoyang area and based on formulizing feature of geologic structure, water supply and hybrid process of superficial coldwater and genetic analysis.
针对赤峰南部—朝阳地区地热田中低温对流型地热系统,在研究其地质构造、水源补给、浅部冷水混合作用影响等特征及其成因的基础上,建立了该区地热田成因的地质模式。
3) origin of geothermal water
地热水成因
4) hot island cause
热岛成因
5) hydrothermal origin
热水成因
1.
There occurred abundant cherts of Mesozoic and Cenozoic Age in south Tibet, the layered, laminated, massive and breccia structures indicate that the cherts are hydrothermal origin.
西藏南部地区广泛发育中、新生代硅质岩,具有层状构造、纹理状构造、块状构造和角砾状等典型古热水沉积构造,其Al/(Al+Fe+Mn)比值、Co/Ni比值、Fe/Ti比值、氧同位素以及TiO2-Al2O3图解等地球化学特征显示为热水成因。
6) thermal mechanism
热力成因
补充资料：传导型地热系统
传导型地热系统
conductive geothermal system
表2中国地热资源表(盆地型，以传导为主的中低温地热资源)┌─┬──────────┬────┬───┬──┬──┬──┬────┬─────┬───────┬──────────┐│地│盆地名称 │地热田 │地温 │热储│热储│可采│岩石与水│ 能刁│FlJ用的地热亏 │苍源(<200Om) ││区│ │ 面积 │梯度 │温度│层厚│系数│的比容 │ 总量 │厂不砰一 │ 折合燃料、动力 ││ │ │(kmz) │(C/ │(C) │(m) │(%) │ (kJ/ │(IO12kJ) │{(’。‘乙kJ) │lo6t标煤{1。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条