Volume 25 Issue 5
Oct.  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(5): 962-980
LYU Guxian, 2019. RESEARCH ON TECTONIC DYNAMO-PETROGENESIS AND METALLOGENESIS AND TECTONOPHYSICOCHEMISTRY. Journal of Geomechanics, 25 (5): 962-980. DOI: 10.12090/j.issn.1006-6616.2019.25.05.079
Citation: LYU Guxian, 2019. RESEARCH ON TECTONIC DYNAMO-PETROGENESIS AND METALLOGENESIS AND TECTONOPHYSICOCHEMISTRY. Journal of Geomechanics, 25 (5): 962-980. DOI: 10.12090/j.issn.1006-6616.2019.25.05.079
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RESEARCH ON TECTONIC DYNAMO-PETROGENESIS AND METALLOGENESIS AND TECTONOPHYSICOCHEMISTRY

doi: 10.12090/j.issn.1006-6616.2019.25.05.079

  • Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

More Information
  • Received: 2019-09-16
  • Revised: 2019-09-30
  • Published: 2019-10-31
    Abstract
  • The theory of "dynamo-petrogenesis and metallogenesis" was proposed in the early 1970s~1980s on the basis of research in the field of tectonogeochemistry such as stress minerals, rock deformation-metamorphism relation and structural control on ore. It represents a significant progress in the aspect of research on structural control on ore in geomechanics field. Applying "tectonic-lithofacies zone", i.e., the carrier of dynamo-petrogenesis and metallogenesis, great breakthroughs have been made in deep ore prospecting of the Shaertuohai chromite deposit, Xinjiang. Subsequent research has developed from the stage of "dynamo-petrogenesis and metallogenesis" to the present-day "tectonophysicochemistry" stage. Based on solid mechanics, research indicates that deformed rocks are formed by deviatoric stress field, which can be divided into differential stress and isotropic stress sections; the latter is named as "additional tectonic hydrostatic pressure". As a physicochemical variable, it can not only arouse rock volume variation but also can affect the chemical equilibrium. Combined with the long-term research on gold deposits in eastern Shandong, it was found that element geochemical distribution is a result of chemical equilibrium and physical chemistry is the cause of chemical action; accordingly, the thought of "The chemical equilibrium is affected by the change of pressure and temperature of tectonic forces" is proposed. The method of "structural correction based on ore-forming depth" has demonstrated the existence of the predicated "secondary enrichment zone" in gold deposits in eastern Shandong, promoting eastern Shandong to become the global third largest gold field from a crisis-mine severely afflicted area. Over more than 40 years' theoretical research, geological survey and prospecting practice, great progress has been made in tectonophysicochemistry. In 1996, the Professional Committee of Geomechanics set up the "Tectonophysicochemistry Professional Group". In 2018, "the Professional Committee of Tectonophysicochemistry" was approved by Chinese Geophysical Society.

     

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