GEOTHERMAL RESOURCES

in

CHINA

January 1996

Prepared by:

Anthony Taylor

Zheng Li

Bob Lawrence & Associates, Inc.

424 N. Washington Street

Alexandria, VA 22314


Geothermal Resources in China — BL&A page 2

INTRODUCTION

In recent years China has experienced rapid economic expansion as it endeavors to bring about a

modern standard of living for its huge population. The GNP grew at an average rate of 9.5%

during the decade of the 80's; and 13%, in 1992 and ‘93. Certain Special Economic Zones in

southern China have raced at over 20% per year recently. These trends are expected to continue,

at least for the next few years.

Growth in the economy has brought a demand for new infrastructure. Additional electrical

generating capacity is needed, both to meet the needs of new industries and the growing middle

class of consumers as well as to close a persistent gap between supply and demand. The Ministry

of Electrical Power in Beijing announced an ambitious goal of installing 100 to 130 GW of new

generating capacity by the year 2000. To achieve this goal, the Chinese will have to increase

capacity at a rate that is more than four times the present level of expansion in the US.

Most of the new capacity will be provided using coal-fired steam turbine systems in the 300 to

600 MW range, thereby further increasing an already-heavy reliance on coal for energy

production. Furthermore, the Ministry of Electrical Power projects that the percentage of annual

coal production (currently 1.1 billion tons) devoted to electrical generation will rise from 29% to

60% by 2010.

Growth in coal consumption will come with a price of increased overall air emissions. There may

be some local mitigation, however, as urban centers convert their space heating needs to

electricity and away from coal burning, which is the primary cause of urban air pollution today.

There is significant and growing interest in China in developing alternative energy sources, both to

meet the demand and to relieve environmental problems. In response to the United Nations

Conference on Environment and Development, held in Brazil during June 1992, China published 

“Agenda 21 - A White Paper on China’s Population, Environment, and Development in the 21st

Century.” This plan was adopted by the State Council of the People’s Republic of China in

March 1994. The key provisions affecting geothermal energy are as follows:

• Give priority to the development of renewable energy sources in the national

energy development strategy. Adopt appropriate financial incentives and market

mechanisms to increase national financial inputs into the development of renewable

energy resources and encourage the participation of local governments and end

users.
Geothermal Resources in China — BL&A page 3

• Conduct a nationwide investigation and assessment of geothermal resources. 

Build geothermal stations. In the process of developing geothermal resources,

protect the environment against adverse impacts.

• Keep up with scientific and technical advances in the world. Strengthen research

on technologies for using new and renewable energy resources. Introduce

advanced foreign technology, improve research conditions, and enhance the

research capabilities of scientific researchers.

• International cooperation in this program will include the use of foreign capital and

technology to conduct research on and build demonstration projects for the

development and use of new and renewable energy resources.

This report is a survey of the results to date of efforts by Chinese geologists and others to identify

and characterize geothermal resources in China. The report is based on documentation available

worldwide, especially from Chinese institutes and governmental agencies, US data bases and the

international geothermal community.

OVERVIEW

Geothermal resources in China are abundant and widely distributed throughout the country. 

There are over 2,700 hot springs occurring at the surface, with a temperature exceeding 250C (S.

Huang et al, 1993). For centuries the Chinese have used hot spring water for therapeutic,

recreational and agricultural purposes. More recently geothermal resources have been applied to

various industrial processes, fish farming and space heating. In 1990, the total flow rate of

thermal water for direct uses amounted to over 9,500 kg/sec (Wang et al, 1990), making China

the second largest direct user of geothermal energy in the world.

Since the early 1970's, recognizing the importance of geothermal energy as an alternative and

renewable energy source, China has conducted extensive explorations aimed at identifying high

temperature resources for electrical generation. To date 181 geothermal systems have been found

on mainland China, with an estimated generation potential of 1,740 MW (Chen et al, 1994). The

estimated potential for Taiwan is 100 MW. Only seven plants, with a total capacity of 32 MW,

have been constructed and are operating currently. Most of these are located in the remote

southwestern area of the country or on Taiwan.
Geothermal Resources in China — BL&A page 4

GEOLOGICAL FEATURES

China is located in the southeastern corner of the Eurasian Tectonic Plate. It is influenced both by

the Pacific Plate to the east and the Indian-Australian Plate to the south. Two geothermal belts

are formed at the juncture of these plates. The Himalayan Geothermal Belt, which is the eastern

extension of the Mediterranean Belt, passes through southern Tibet and western Sichuan

Provinces, turns southward through western Yunnan Province and then extends downward

through Thailand. The Circum-Pacific Belt passes through eastern Taiwan. (See Fig. 1) The

Himalayan Belt within China is extensive, measuring more than 2,800 km long and 200-400 km

wide. There are 112 known geothermal systems in southern Tibet; 12, in western Sichuan; and

47, in western Yunnan (Ren et al, 1995).

Heat flow (the rate of conductive heat loss from the earth’s interior through a unit area of surface)

is a direct surface indication of the thermal regime at depth. As such it is a useful tool in

exploring for geothermal energy resources. The geothermal background in China is closely

related to tectonic factors. Generally the younger and more active regions have the highest

geothermal background. Overall the heat flow pattern in China is characterized as high in the

south and east and low in the west and north. For example, southern Tibet, western Sichuan and

Yunnan, and Taiwan are active tectonic areas from the Cenozoic Age. Heat flow studies (Wang

and Huang, 1990) found the average heat flow in southern Tibet is in the range 80 - 100 mW/m2

and for the Tengchong volcanic area in western Yunnan >80 mW/m2 (Wang et al., 1990). Heat

flow values in the east are relatively high (60 - 70 mW/m2). In contrast, values in the west are low

(<50 mW/m2). Taiwan is generally characterized by high heat flow (>80 mW/m2) and in its high

temperature geothermal areas, heat flow is >120 mW/m2 (Lee and Cheng, 1994). The reason for

these geographical disparities is that since the Mesozoic Age, China has been strongly influenced

by the tectonic forces from the south and east mentioned above, creating hot regions in these

areas.

Geothermal resources in China can be divided into three types, each with two subtypes (Huang,

et. al., 1993). Subtype Ia is associated with recent volcanic eruption; subtype Ib, with recent

magmatic intrusion. These are the high temperature resources. Subtypes IIa and b are associated

with interplate uplifted areas of the Earth’s crust. Subtypes IIIa and b are associated with

subsided areas of the Earth’s crust. The heat sources for IIa, IIb and IIIa are related to the deep

circulating convection of underground water. The heat source of IIIb depends on heat

conduction.

Hot springs, a common manifestation of underlying geothermal resources, are widespread in

China and have been used for a variety of purposes over many centuries. Since the early 1970s

there has been an intensive effort to study and catalog the hot springs, with a view toward solving
Geothermal Resources in China — BL&A page 5

the energy shortage problem. A data base, developed by the Institute of Geology of the Academy

of Science, currently contains information on 2,509 hot springs with a temperature >250 C (Xiong

et al, 1995). The information includes location, temperature, flow rate, water chemistry,

geological setting and average ground temperature at a depth of 0.8 m. Statistics of the data base

are summarized below.

HOT SPRINGS IN CHINA

Province Number Temperature (0C) Heat Discharge

(103 J/s)

25-40 40-60 60-85 >85

Yunnan 823 341 323 129 30 682507.00

Xizang 271 51 97 88 35 622928.90

Sichuan 240 89 118 27 6 335281.50

Guangdong 285 81 125 68 11 150645.72

Fujian 177 41 81 51 4 101609.01

Hunan 108 74 31 2 1 98700.26

Taiwan 78 7 27 31 13 93500.47

Xian 14 8 6 0 0 80694.53

Hubei 52 30 15 7 0 68080.75

Qinghai 39 20 10 6 3 64725.62

Gansu 14 8 6 0 0 61851.92

Jiangxi 79 34 32 13 0 51159.79

Guizhou 58 40 18 0 0 37838.52

Jiangsu 7 3 3 1 0 33669.80

Xinjiang 56 23 23 6 4 28330.03

Henan 23 11 7 5 0 24817.53

Guangxi 36 19 12 5 0 21131.21

Anhui 17 8 7 2 0 20465.94
Province Number Temperature (0C) Heat Discharge

(103 J/s)

Geothermal Resources in China — BL&A page 6

Hainan 34 7 14 12 1 18469.45

Jilin 5 2 1 2 0 17973.05

Hebei 27 6 12 8 1 17285.14

Liaoning 27 11 11 5 0 13596.11

Shandong 17 2 8 5 2 10751.39

Taiyuan 5 3 1 1 0 3926.66

Inner Mongolia 3 0 2 0 1 3746.00

Zhejiang 14 13 0 1 0 1180.10

Total 2509 932 990 475 112 2664866.40

The data show that nearly 70% of China’s hot springs are located in five provinces, Fujian,

Guangdong, Yunnan, Sichuan and Tibet. Note that hot springs in the lower temperature ranges

are distributed widely, while the highest temperature springs are found largely in Yunnan, Tibet,

and Guangdong on the mainland and in Taiwan.

HIGH TEMPERATURE GEOTHERMAL RESOURCES (>1500 C)

High temperature geothermal resources are concentrated in recent volcanic and tectonically active

regions. In southern Tibet there are over 600 hydrothermal manifestations, including geysers,

hydrothermal explosions, steaming grounds, fumaroles, and boiling springs. The estimated

reservoir temperatures vary from 170 to 2700 C. The total natural heat discharge at the surface is

4,900 x 1013 J/a (Shen and Chen, 1994). High temperature geothermal fields in Tibet are located

mostly along the two sides of the Yarlung zangbo River, which runs along the junction of the

Eurasian and Indian Plates.

Yunnan is the province with the most hydrothermal features. Over 900 hot springs have been

discovered, concentrated largely in the western part of the province on the border with Burma,

around Tengchong township. This is also an area, like southern Tibet, having few conventional

energy resources.
Geothermal Resources in China — BL&A page 7

Western Sichuan Province is an area of highlands and mountains. Twelve high temperature

geothermal systems have been discovered, but are used only for extraction of salts at this time.

About 80 hot springs and fumarolic areas have been discovered in Taiwan. Such geothermal

manifestations are associated with the Pacific Ring of Fire and are related to volcanic activity of

the late Cenozoic Age.

LOW-MEDIUM TEMPERATURE GEOTHERMAL RESOURCES (<1500 C)

China has a large number of low-medium temperature geothermal resources, used extensively for

non-electrical, direct purposes such as space heating, agriculture, fish farming and industrial

processing. There are two types of low-medium temperature resources. The first are convective

type geothermal systems, not heated by young magma bodies, but rather by circulation of the

water at depth. Generally the deeper the water the higher the temperature. Geothermal resources

of this type exist mainly in three areas (see Fig. 1):

1. The Southeast Coast Low-Medium Temperature Geothermal Belt - This belt

traverses Fujian, Guangdong, Eastern Jiangxi and Southern Hunan Provinces in the

southeastern part of the country. Over 600 hot springs, mostly with temperatures

in the range 40 - 800 C, have been discovered. There are 26 systems with

temperatures 80 - 950 C. In 1970 a 286 kW experimental power station,

consisting of two units, was constructed in this area at Dengwu, Guangdong

Province. The plant continues in operation today, although at low efficiency due

to the low fluid temperature (910 C).

2. The E. Shandong/E. Liaoning Peninsula Geothermal Belt - This belt lies to the east

of Beijing and has about 70 hot springs. Temperatures are in the range 40 - 700 C,

with a few as high as 900 C. In 1977 a 100 kW experimental power plant was built

on the Liaoning Peninsula at Yingkou. It was shut down several years ago.

3. The Fen/Wei graben area to the west of Beijing - The pattern of hot springs is “S”

shaped, conforming to the graben. Temperatures in the northern and southern

parts are higher (60 -800 C); in the middle, lower (40 - 600 C), probably reflecting

different circulation at depth. In 1971 a 200 kW experimental power plant was

built at Huailai in Hebei Province. It has since been shut down.

The second type of low-medium temperature geothermal resource is thermal water associated

with conductive systems in large sedimentary basins (see Fig 1). Basins are a prominent feature in
Geothermal Resources in China — BL&A page 8

China, comprising 36 % of the country. Nine basins in eastern and central China have been found

to have large geothermal resources. They include Song-Liao, Lower Liaohe, North China,

Northern Jiangsu, Feng-Wei, Ordos, Sichuan, Lei-Qiong and Chuxiong. The recoverable thermal

water in these basins is equivalent to 1.8 billion tons of coal (Wang, 1995). The recoverable

resources in North China and Northern Jinansu Basins make up 73 % of this total. For this

reason, these two areas are the most promising for development of low-medium temperature

geothermal resources in China. Feng-Wei and Lei-Qiong Basins are small, but are promising for

development because the water quality is good and the flow rate is satisfactory for exploitation. 

Except for Chuxiong Basin, the water quality in the other Mesozioc Age basins such as Sichuan,

Ordos and Song-Liao appears to be poor and not promising for development. Basins in western

China such as Tarim, Chaidamu and Zhungeer offer little promise because of poor water quality,

including high salinity.

PRINCIPAL GEOTHERMAL FIELDS (POWER GENERATION)

Province Field Area

km2

Potential

MW

Installed

MW

Reservoir T

0C

Tibet Yangbajian 15 25.18 329

@ 2000 m

Naqu 10 3-4 1.0 170

Yangyi 11 30 0 207

@ 312 m

Langjui 1 10 2.0 180

Yunnan Rehai 10 0 230 - 275

Lanpu 4.5 0 160 - 220

Ruidian 3.2 0 190

Ruili 12 0 215 - 227

Sichuan Litang 10 0 190 - 220

Taiwan Qingshui 3.0 230

@ 3000 m

Tuchang 0.3 173
Province Field Area

km2

Potential

MW

Installed

MW

Reservoir T

0C

Geothermal Resources in China — BL&A page 9

Tatun 100 0 293

Yangbajian — Located 90 km to the northwest of Lhasa City, capital of Tibet. The field has a

total area of about 15 km2 , although the accessible part of the upper reservoir from which hot

fluids can be produced covers only about 4 km2. The field is controlled by a crisscross of fault

systems. There are three northeast compression shear faults and three perpendicular northwest

tension shear faults to form the boundaries of the field. There is dense and hard granite in the

basement of Yangbajian. The faults extend deep into the reservoir and there are basement faults

passing through the reservoir. The hot water flows up along the faults in the basement to the

Quaternary grit layer to form a shallow reservoir.

Exploration of the shallow reservoir was conducted during the years 1976-84. The electrical

generation potential was estimated at 34 kW. Installed capacity has grown from an initial 1 MW

unit in 1977 to 25 MW currently, generated by nine single flash, double flash and hybrid cycle

power plants. Fluid flows from 18 wells approximately 200 m deep. The temperature range is

140 - 1600 C. Yangbajian provides 41 % of the electrical needs of Lhasa City, 60 % in winter. 

Waste thermal water has been used to heat greenhouses with floor space of 50,000 m2.

In 1993, the first deep wells were drilled at Yangbajing. A temperature of 3300 C was recorded in

one of the wells at a depth of 2,000 m. The generation potential of this single well has been

estimated at 10 MW (Ren et al, 1995). This success led to a prediction that Yangbajian capacity

would reach 50 -60 MW by 2000 and 120 - 160 MW by 2020.

Langjui — Located in the far western part of Tibet. The field has an explored area of only 1

km2. In the early 1980s, 13 wells were drilled within this area. Temperatures were 100 -1050 C. 

The initial estimate of capacity was 10 MW, although this number has probably been reduced

because of downward leakage of cold water which damaged part of the geothermal reservoir. 

Since 1987 there has been a 2 MW plant in intermittent operation at Langjui.

Naqu — Located near the town of Naqu, about 300 km north of the capital of Tibet, at an

elevation of 4500 m. Exploratory drilling, beginning in 1984, located a 0.6 km2 shallow reservoir

with temperatures up to 1700 C. The area heated by concealed shallow flows is about 10 km2. In

1993, the Government of Tibet, with the aid of the UN Development Program, installed a 1 MW,

binary cycle plant, using an Ormat Energy Converter. Successful operation of this plant over time
Geothermal Resources in China — BL&A page 10

will serve as a demonstration of this approach to supplying the electrical needs of numerous towns

on the Tibetan Plateau.

Yangyi — Located 45 km southwest of Yangbajian, at an elevation of 4,550 m. Fifteen wells

(0.3 - 1.1 km) have been drilled, outlining a small (1.6 km2) upflow center, probably caused by the

intersection of fracture zones. Reservoir temperatures as high as 2070 C were measured within

this area. At the time, this was the first instance of a downhole temperature above 2000 C on

mainland China. Surface manifestations associated with shallow, migrating fluids cover an area of

about 11 km2. The water quality is good. The concentration of CO2 is relatively low, despite the

significant presence of non-condensable gas in the water. Problems from CaCO3 scaling should

be minimal.

Parameters of the geothermal reservoir proved to be stable. Temperature, pressure and flow rate

were stable during almost 900 hours of testing in the early 1990s. The estimated generation

capacity is 30 MW. Development of the Yangyi Field, initially with 10 MW, is a high priority of

the Chinese geothermal community.

Rehai — Located 11 km southwest of Tengchong township in the westernmost part of Yunnan

Provence, near the border with Burma. Strong hydrothermal manifestations, which include

boiling springs, fumaroles and steaming ground, cover an area of about 10 km2. Geophysical

measurements indicate the crustal layer beneath the surface of this field is only about 7 km thick. 

Away from the center, the thickness of this layer gradually increases, taking the shape of an

umbrella and providing conditions for the formation of a geothermal reservoir or a magma

chamber. Thirteen shallow test holes, ranging in depth from 100 to 400 m, were drilled during the

period 1976 to 1992. Based on measurements from these and other information, it is possible to

say that Rehai is a hot water system with a magmatic heat source of about 400 to 6000 C. The

reservoir temperature is estimated to be 230 to 2750 C. The electric generation potential cannot

be estimated accurately due to a lack of adequate drill holes, but the field may be one of the

richest in China.

Lanpu — Located 10 km south of Rehai and usually considered part of Rehai. The area of the

geothermal field is about 4.5 km2. The reservoir temperature is estimated to be in the range 160

to 2200 C.

Ruidian — Located 60 km north of Tengchong township in Yunnan Province. The field has an

area of about 3 km2 and an estimated reservoir temperature of 1900 C.

Ruili — Located on the bank of the LiJiang River near Ruili City, which is an important

southwestern commercial and trading port on the border with Burma, about 100 km south of
Geothermal Resources in China — BL&A page 11

Tengchong. The field is 12 km2 in size. Reservoir temperatures are in the range, 215 to 2300 C. 

This field is also high on the priority list for development, most likely with an initial plant of 3 -5

MW capacity.

Litang — Several small fields located in western Sichuan Province, near Litang township. 

Reservoir temperatures are in the range, 190 to 2200 C. The electric generation potential is

probably less than 10 MW because of the limited reservoir area.

Qingshui — Located in east Taiwan. Seven productive boreholes have been made, the deepest

about 3,000 m. Downhole temperatures as high as 2300 C have been recorded. In 1981 an

experimental, single flash power plant, with 3 MW capacity, was constructed.

Tuchang — Located in east Taiwan. The field lies in a slate formation. Reservoir temperature,

at 445 m, is 1730 C. In 1985 an experimental, binary cycle power plant, with 0.3 MW capacity,

was built.

Tatun — Located in east Taiwan. The field lies in a volcanic region. Exploration of a deep

reservoir (1500 m) has found temperatures up to 2930 C. The estimated generation capacity is

about 100 MW.

OUTLOOK FOR DEVELOPMENT

China has several problems impacting the prospects for development. Among these are the

uneven distribution of geothermal resources. High temperature resources are concentrated in

Tibet, W. Yunnan, and W. Sichuan Provinces along the Himalayan Geothermal Belt. Lowmedium temperature resources are widespread in large scale sedimentary basins. However,

thermal water in basins from western China has little promise because of high salinity. Another

problem is a lack of accurate assessments of geothermal resources for the whole country.

A shortage of indigenous investment capital is also a problem. Exploration and development of

geothermal resources is expensive and bears risks. China does not have the large amounts of

money needed. It would welcome either foreign investment of formation of joint ventures, in the

form of either build-operate-own or build-operate-transfer. Prelininary analysis has shown that,

for a 10 MW geothermal power plant, the time for investment recovery will be more than 5 years

in Tibet and up to 6 years in W. Yunnan (Ren et al, 1995).

Finally there are technical problems that must be overcome. Corrosion and scaling are two

common issues in the use of geothermal resources. In the Yangbajing geothermal field, these
Geothermal Resources in China — BL&A page 12

conditions are especially serious. Better resevoir engineering is also needed. Reinjection of fluid

back into the resevoir is important both for efficient use of the resource and for environmental

reasons. Unfortunately this is not done in most cases. For direct uses, better heat exchange

technology is needed. Although some research on heat exchangers and heat pumps has been done

in China, it has not been applied to production units.

Chinese planners have identified a need to meet a persistent electric generation shortfall in remote

regions such as the Tibetan Plateau, western Sichuan and western Yunnan Provinces. Geothermal

energy is attractive because there is little fossil fuel and the national and regional electric grids do

not reach these areas.

The geothermal community sees the priority tasks as follows:

• Accelerate the exploration and use of the deep reservoirs at Yangbajing. The

objective would be to meet the electric needs of the Lhasa area.

• Develop the Yangyi Geothermal Field with a modern 10 MW-size power plant.

• Explore the deep reservoirs in the Naqu Field and expand the existing installed

capacity.

• Establish a 3 - 5 MW pilot project at the Ruili Geothermal Field, followed by

development of the Rehai Field with a 10 MW plant.

• Develop the fields around Litang in western Sichuan.

DIRECT USE

China is the second largest user of geothermal energy for non-electrical purposes. Thermal water

is used directly for industrial and agricultural processes such as dyeing, drying of fruits and

vegetables, paper and hide processing, air conditioning, and preheating boiler feed water. Four

provinces are the most active in their use of geothermal resources for direct uses, Hebei, Tianjin,

Shandong, and Tibet.

Space heating is a common application in Norht China where over 1.3 million m2 of floor space is

heated. The largest project is in Tianjin where about 50 wells provide thermal water with

temperatures up to 970 C to heat a total area of 805,000 m2. Space heating projects in Beijing are

spread over a large area of the city, although there are no large central heating systems.
Geothermal Resources in China — BL&A page 13

Greenhouses are also major users of geothermal energy. In 1990 China had about 1.2 million m2

of geothermally heated greenhouse space in 17 provinces, with Hebei Province accounting for the

largest share.

Fish farming is another rapidly growing application. There are over 1.6 million m2 of fish ponds in

17 provinces. The projects include African carp, eels, shrimp, turtles and snails.

Medical treatment and tourism are the oldest applictions of termal water. In recent years the use

of hot spring resources for medical treatment and tourism has developed rapidly. The number of

sanatoria in China is over 200. Reportedly there are about 600 baths and 23 swimming pools.
Geothermal Resources in China — BL&A page 14

REFERENCES

Chen Mo-xiang, Wang Ji-yang, and Deng Xiao, Geothermal Systems in China - Formation,

Characteristics and Potential Evaluation (in Chinese), Science Press, Beijing, 1994.

Chen Mo-xiang, A New Map of Hot Spring Distribution in China and its Explanation, Scientia

Geologica Sinica, Vol 2, No 1, 1993.

China’s Agenda 21 - White Paper on China’s Population, Environment, and Development in the

21st Century, Beijing, 1994.

Guo Guoying, Exploitation Prospects of Geothermal Resources in Hengduan Mountains, China,

in Proceedings of the World Geothermal Congrsss, 1995.

Hu Baigeng, Reservoir Simulation of the Yangbajian Geothermal Field in Tibet, China, in

Proceedings of the World Geothermal Congress, 1995.

Huang Shang-yao and Zheng Keyan, The Latest Progress in Exploration and Utilization of

Geothermal Resources in China, in Proceedings of the World Geothermal Congress, 1995.

Huang Shao-ping and Wang Ji-yang, Heat Flow Distribution and Thermal Structure of the

Continental Area of China, in Advances in Geoscience, China Ocean Press, Beijing, 1992.

Huang Shang-yao Ma Da-le, and Liu Te-ying, The 1.6 M Distribution Map of Hot Springs in

China, in Explanation and Nomenclature of Hot Springs in China (in Chinese), China Geographic

Publishing House, Beijing.

Liao Zhi-jie, A Review of the Rehai (Hot Sea) Geothermal System in Tengchong County, Yunnan

Province, China, in Proceedings of the World Geothermal Congress. 1995.

Pollack H N, Surter SJ, and Jhonson JR, Heat Flow from the Earth’s Interior: Analysis of the

Global Data Set, in Review of Geophysics, Vol 31, 1993.

Ren Xiang, Zhang Zhenbguao, Tang Ninghua, and Wu Fangzhi, The Strategy and Program on

Geothermal Electric Generation by the Years 2000 and 2020 in China, in Proceedings of the

World Geothermal Congress, 1995.

Ren Xiang, Summary of 1993's Work of China Geothermal Association, in Report for Energy

Resource Association of China (in Chinese), Beijing, 1993.
Geothermal Resources in China — BL&A page 15

Tong Wei and Zhang Ming-tao, Geothermics in Tengchong, Science Press, Beijing, 1989.

Wang Ji-yang, Chen Mo-xiang, Siong Liang-ping, and Pang Zhong-he, Geothermal Resources

and Development in China, in Proceedings of the World Geothrmal Congress, 1995.

Wang Ji-yang, Geothermal Energy in Developing Countries - Prospects and Problems, A Case

History from China, in Proceedings of the World Geothermal Congress, 1995.

Wang Ji-yang, Huang Shao-peng, and Chen Mo-xiang, Explanitory Note of the Terrestrial Heat

Flow Map of China, in Geophyusical Atlas of China, Science Press, Beijing, 1995.

Wang Ji-yang, Xiong Liang-ping, and Chen Mo-xiang, Nature of Hydrothermal Systems and

Geothermal Resources in Coastal Area of China, in Geothermal Reources in China, Science Press,

Beijing, 1994.

Wang Ji-yang, Chen Mo-xiang Xiong Liang-ping etc., Geothermal Systems in Continental Area of

China, in Water-Rock Interaction, Balkema, Rotterdam, 1992.

Wang Ji-yang, Xu Qing, and Zhang Wen-ren, Heat Flow and Some Geologo-geothermal

Problems in Yunnan Province, in Science and Geology, Vol 12, No 4, 1990.

Wang Daichang and Qin Chang-long, Yangbajian Geothermal Field in Tibet (in Chinese), Tibet

People’s Publishing House, Lhasa, 1989.

Wang Ji-yang, Chen Mo-xiang, etd., Geothermal Studies in China, in Journal of Volcanology and

Geothermal Research, Elseveir Scientific Publishing Co., Amsterdam, 1981.

Xiong Liang-ping, Liu Jie, He Li-juan, Hu Shen-biao, and Wang Ji-yang, Heat Flow and Hot

Spring Data Base in China and Compliation of Geothermal Map Set by Computer, in Proceedings

of the World Geothermal Congress, 1995.

Xiong Liang-ping and Lin Jin-xuan, Geothrmal Resources Database System, Seismological Press,

Beijing, 1993.

Xiong Liang-ping and Lin Jin-xuan, The First Geothermal Resources Database in China, in

Geothermal Resources Council Transactions, Vol 15, 1991.

Zheng Keyan and Cao Jinrong, Growth of Geothermal District Heating in China, Proceedings of

the World Geothermal Congress, 1995.