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1982 Vol. 1, No. 2

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THE GEOMORPHOLOGICAL REGULARITIES OF KARST WATER OCCURENCES IN GUIZHOU PLATEAU
Yang Mingde
1982, 1(2): 81-91.
Abstract PDF(669KB) icon1777 icon678
Abstract:
The Guizhou Plateau is situated in the subtropical zone of southwest China.The Plateau has been uplifted strongly since the Quaternary period. Carbonate rocks are widely distributed and karst is well developed,forming typical features over the plateau. The conditions for karst water occurences are v...
SOLUTIONAL FEATURES OF LIMESTONE CAVES IN GUILIN AREA
Zhu Xuewen
1982, 1(2): 93-103.
Abstract PDF(2715KB) icon1916 icon713
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In this paper the speleogens of limestone caves in the famous Guilin karst peak-forest area are discussed, and a classification proposed. The solutional patterns in the caves can be divided according to their morphologic characteristics into five basic types: orientational flow mark type, pocket typ...
A PRELIMINARY STUDY ON THE SUBTERRANEAN STREAM SYSTEMS OF LUOTA AREA, HUNAN PROVINCE
Yu Haoran, Wu Yinke, He Weixin, Liu Haiqing
1982, 1(2): 105-117.
Abstract PDF(765KB) icon1596 icon718
Abstract:
The Luota Area in Northwestern part of Hunan Province is a synclinal confluence basin of bare karst. It has a special hydrogeological structure composed by several karstified aquifers which are connected, but in some cases separated each other by non-soluble beds ( Multi-aquifer). There are many sub...
RECESSION EQUATION AND ITS APPLICATION——CASE HISTORY OF LUOTA KARST BASIN
Huang Jingxi
1982, 1(2): 118-126.
Abstract PDF(495KB) icon1581 icon664
Abstract:
In this paper the Luota Karst Basin is taken as an example to verify the nonuniformity of karst water-bearing medium, and derive the recession equation of discharge as which can be used as a method to estimate the karst ground water resources. Based on the long-term observation of the water points i...
EVOLUTION OF PEAK CLUSTER-DEPRESSION IN GUILIN AREA AND MORPHOMETRIC MEASUREMENT
Zhu Dehau
1982, 1(2): 127-134.
Abstract PDF(533KB) icon1840 icon674
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Developed in Guilin area are typical tropical karst landform of peak forests, which may be classified into two major types: peak cluster-depression type and peak forest-plain type. An attempt is made to carry out morphometric measurements and statistic analyses on one hundred and eighty-two polygona...
SOME CHARACTERISTICS OF KARST WATER IN NORTH CHINA
He Yubin
1982, 1(2): 135-142.
Abstract PDF(481KB) icon1705 icon719
Abstract:
In North China, karst features occur mainly in Hebei, Shanxi, South Liaoning, northern parts of Shandong and Henan, and Shanxi Provinces, extending to the north of the line from the Qingling mountain range to the Huaihe River. The terrain belongs to a semi-arid and semi-humid warm temperate zone. Ka...
DISCUSSION ON THE GENESIS OF THE LATERITE IN GUIXIAN, GUANGXI
Peng Datian, Zhao Xinye, Luo Zhonguo
1982, 1(2): 143-151.
Abstract PDF(500KB) icon1835 icon670
Abstract:
The genesis of laterite is still a controversial problem. According to the geological profile, grain size, minerals and chemical composition of the laterite in a studied area in Guixian, Guangxi, the authors consider that the laterite there belongs to the sedentary-slope wash deposition. The materia...
THE COINCIDENT SPECTRAL PLOT METHOD FOR SELECTING THE OPTIMAL REMOTE SENSING BANDS OF CARBONATE ROCKS
Shu Shourong
1982, 1(2): 152-157.
Abstract PDF(446KB) icon1692 icon579
Abstract:
The selection of the optimal remote sensing bands of carbonate rocks is an important problem in the remote sensing studies of karst geology. Although the statistical method is a strict mathematical method for selecting the optimal remote sensing bands, it is quite sophisticated in calculation and mu...
1982, 1(2): 159-162.
Abstract PDF(317KB) icon1670 icon618
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1982, 1(2): 163-166.
Abstract PDF(306KB) icon1595 icon667
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