Nappe structure, as was first discovered by the authors during the regional geological survey at the scale of 1:50,000 in The Jinggang Mountain, is mainly comprised of a series of NNE-NE-striking thrust fault zones an...Nappe structure, as was first discovered by the authors during the regional geological survey at the scale of 1:50,000 in The Jinggang Mountain, is mainly comprised of a series of NNE-NE-striking thrust fault zones and thrust sheets among them. Sinian, Cambrian, Ordovician, Devonian, Carboniferous,Triassic, Jurassic and Cretaceous strata are involved in the thrust nappe system. The nappe structure is of the type of duplex structures formed as a result of the earlier stage migration from SE to NW and late stage migration from E to W of sedimentary cover or basement strata. Formation of the nappe structure in the studied area involves two main epochs: Early Yanshanian and Late Yanshanian to Early Himalayan. The mineral deposits and the buried coalfields in the area, especially the latter, are extensively controlled by the nappe structure.展开更多
THE Jinggang Mountains are located in the southwestern part of Jiangxi Province, the middle section of the Luoxiao mountain chain along the border between Hunan and Jiangxi provinces. It is the cradle of the Chinese r...THE Jinggang Mountains are located in the southwestern part of Jiangxi Province, the middle section of the Luoxiao mountain chain along the border between Hunan and Jiangxi provinces. It is the cradle of the Chinese revolution, and has as many as 29 historical revolutionary sites. It is also an ideal place for sightseeing, attracting tourists with its mountains, waterfalls and forests. The city of Jinggangshan is located in the midst of the mountains, 1,000 meters above sea level. It has the lowest population density of any city in China,展开更多
Mao Zedong lived in this house in Dajing Village at the time he led his troops to the Jinggang Mountains after the Autumn Harvest Uprising on October 24, 1927.
基金supported by a grant from the Ministry of Land and Resources(Project No:19961300002011)for the regional geological survey of the Jinggangshan City section,Yaqian section,Tianhe section,Nashan section of the 1:50,000 geologic mapa key orientation grant(No.KZCXZ-SW-117)of CAS Knowledge Innovation Project for the constitution,structure and evolution of the geotectonic systems of South China Sea and its adjacent regions.
文摘Nappe structure, as was first discovered by the authors during the regional geological survey at the scale of 1:50,000 in The Jinggang Mountain, is mainly comprised of a series of NNE-NE-striking thrust fault zones and thrust sheets among them. Sinian, Cambrian, Ordovician, Devonian, Carboniferous,Triassic, Jurassic and Cretaceous strata are involved in the thrust nappe system. The nappe structure is of the type of duplex structures formed as a result of the earlier stage migration from SE to NW and late stage migration from E to W of sedimentary cover or basement strata. Formation of the nappe structure in the studied area involves two main epochs: Early Yanshanian and Late Yanshanian to Early Himalayan. The mineral deposits and the buried coalfields in the area, especially the latter, are extensively controlled by the nappe structure.
文摘THE Jinggang Mountains are located in the southwestern part of Jiangxi Province, the middle section of the Luoxiao mountain chain along the border between Hunan and Jiangxi provinces. It is the cradle of the Chinese revolution, and has as many as 29 historical revolutionary sites. It is also an ideal place for sightseeing, attracting tourists with its mountains, waterfalls and forests. The city of Jinggangshan is located in the midst of the mountains, 1,000 meters above sea level. It has the lowest population density of any city in China,
文摘Mao Zedong lived in this house in Dajing Village at the time he led his troops to the Jinggang Mountains after the Autumn Harvest Uprising on October 24, 1927.
