Geothermal Geology Characteristic and Origin Analysis of Shilin Basin in Yunnan Province

Xiao Ling Zhang; Hong Zhan Liu; Kang Chen

doi:10.4028/www.scientific.net/AMR.779-780.1449

Paper Titles

A Review on Biomass Fast Pyrolysis Oil Properties and Applications
p.1431

The Individual WTA Changing Analysis for Eco-Compensation Construction in Water Source Conservation Area
p.1437

Sand Mining Monitoring andAnalysis of the Yangtze River Based on Multi-Beam Bathymetry
p.1441

Groundwater Vulnerability Fuzzy Evaluation in Qujing Basin
p.1445

Geothermal Geology Characteristic and Origin Analysis of Shilin Basin in Yunnan Province
p.1449

Soil Erosion and Preventive Measures in the 3^rd Expansion Project of Xiaolongtan Power-Station
p.1453

The Porous Medium of Ultra-Low Permeability Reservoir has an Effect on Oil Recovery
p.1457

Study on Sediment Reduction Effect by Soil Retaining Dam with Different Storage Capacity Allocation Proportion in Dali River Watershed
p.1462

Energy Saving from Traditional Settlement – A Case Study on Environmental Ideology of Traditional Settlement in Fujian, China
p.1468

HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 779-780Geothermal Geology Characteristic and Origin...

Geothermal Geology Characteristic and Origin Analysis of Shilin Basin in Yunnan Province

Abstract:

based on geothermal anomalies and geothermal wells of Shilin basin, the structure of geothermal reservoirs, geothermal geological characteristics and hydrochemistry of thermal groundwater are examined. Geothermal reservoir of the geothermal field is Proterozoic Sinian dolomite and dolomitic limestone. Characteristic of geothermal water runoff and geothermal field are controlled by Jiuxiang fracture and Niutoushan ancient mainland. The drillings data shows that the temperature gradient is 1.5-4.8°C/100m. Deep circulation is the main origin of geothermal water. The chemical type of geothermal water is HCO₃-Ca, and high silicic acid content. The geothermal water supply is limited from the hydrogeological conditions; we should control the development and utilization.

You might also be interested in these eBooks

Materials, Transportation and Environmental Engineering

View Preview

Info:

Periodical:

Advanced Materials Research (Volumes 779-780)

Pages:

1449-1452

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.779-780.1449

Citation:

Cite this paper

Online since:

September 2013

Authors:

Xiao Ling Zhang, Hong Zhan Liu, Kang Chen

Keywords:

Geologic Genetic Model, Geothermal Reservoir, Geothermal Resource, Shilin Basin

Export:

RIS, BibTeX

Price:

Permissions CCC:

Request Permissions

Permissions PLS:

Request Permissions

Сopyright:

Citation:

References

[1] Xu Shiguang, Chen Lianzhu. Kunming low-temperature geothermal field and its development utilization [J]. Hydrogeology and engineering geology, 2000, (3), 22 -24.

Google Scholar

[2] Xue Chuandong, Liu Xing, Yang Hao etc. Numerical simulation of geothermal groundwater in leaky aquifer system, in Kunming city geothermal field [J]. Advance in earth sciences , 2003, 18(6), 899-905.

Google Scholar

[3] Xue Chuandong, Pu Chuanjie, Liu Xing etc. Numerical simulation for solute transport in karst geothermal groundwater aquifer system in Kunming geothermal field [J]. Carsologica Sinica, 2003, 22(4), 251-257.

Google Scholar

[4] Cheng Xianfeng, Xu Shiguang, Zhang Shitao. Characteristics of geothermal geology and genetic model of the Anning hot spring in Yunnan Province [J]. Hydrogeology and engineering geology, 2008, (5), 124-128.

Google Scholar

[5] Yang Jinhe, Gao Juncai. Geothermal geological feature analysis and research of Anning hot spring[J]. Journal of Kunming University of science and technology(science and technology) , 2008, 33(5), 1-6.

Google Scholar