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KULAKOV A P, QIU Shan-wen, MIASNIKOV E A, WANG Xi-kui, TASHCHI S M, ZHAO Hua-chang, SONG Chang-chun. RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)[J]. Chinese Geographical Science, 2000, 10(4): 348-355.
Citation: KULAKOV A P, QIU Shan-wen, MIASNIKOV E A, WANG Xi-kui, TASHCHI S M, ZHAO Hua-chang, SONG Chang-chun. RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)[J]. Chinese Geographical Science, 2000, 10(4): 348-355.
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RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)

  • 1.

    Pacific Institute of Geography, Vladivostok 690041, Russia;

  • 2.

    Changchun Institute of Geography, the Chinese Academy of Sciences, Changchun 130021, P. R. China;

  • 3.

    Chungchun University of Science and Technology, Chungchun 130061, P. R. China

  • Received Date: 1999-11-22
  • Publish Date: 2000-12-20
  • The"ring-morphostructures"(RM) are the object of this study. They are one of the most significant element of lineament's structure and unknown for the majority of investigations. RM are numerous to lineament's zone:they have different size (from 10-20km to 500-800km in diameter), structure, age, geological history and have been divided into several classes on the most important signs. They have a spatial-genetic connection Amur-Songhua-Huanghe lineament (ASHL) and had been developed simultaneously with it. The RM exerted an essential influence on the geologic-geomorphological structure, evolution and geodynamics of lineament. The main factor of evolution of lineament is a long geological process of extension of the earth's crust which is a result of the expanding earth.
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  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

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RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)

  • 1. Pacific Institute of Geography, Vladivostok 690041, Russia;
  • 2. Changchun Institute of Geography, the Chinese Academy of Sciences, Changchun 130021, P. R. China;
  • 3. Chungchun University of Science and Technology, Chungchun 130061, P. R. China
  • Received Date: 1999-11-22
  • Publish Date: 2000-12-20

Abstract: The"ring-morphostructures"(RM) are the object of this study. They are one of the most significant element of lineament's structure and unknown for the majority of investigations. RM are numerous to lineament's zone:they have different size (from 10-20km to 500-800km in diameter), structure, age, geological history and have been divided into several classes on the most important signs. They have a spatial-genetic connection Amur-Songhua-Huanghe lineament (ASHL) and had been developed simultaneously with it. The RM exerted an essential influence on the geologic-geomorphological structure, evolution and geodynamics of lineament. The main factor of evolution of lineament is a long geological process of extension of the earth's crust which is a result of the expanding earth.

KULAKOV A P, QIU Shan-wen, MIASNIKOV E A, WANG Xi-kui, TASHCHI S M, ZHAO Hua-chang, SONG Chang-chun. RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)[J]. Chinese Geographical Science, 2000, 10(4): 348-355.
Citation: KULAKOV A P, QIU Shan-wen, MIASNIKOV E A, WANG Xi-kui, TASHCHI S M, ZHAO Hua-chang, SONG Chang-chun. RING-MORPHOSTRUCTURES OF THE AMUR-SONGHUA-HUANGHE LINEAMENT (EASTERN MARGIN OF ASIA)[J]. Chinese Geographical Science, 2000, 10(4): 348-355.
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