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《Acta Geological Sinica》 1978-02
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THE MAIN CHARACTERISTICS OF GEOLOGICAL STRUCTURES IN THE CHILIENSHAN REGION, CHINA

Wei Chunhai et al.  
In the Chilienshan region there exist various tectonic systems formed as a result of repeated tectonic movements. They are compounded with one another, thus constituting a complicated tectonic framework. The present paper deals in the main with the Paleo-Hosi system which attained its full growth essentially in the Chilien movement at the end of Silurian. It is made up of a series of parallel fold belts of N55° to 65°W trend and intervening rock masses. It controls the distribution of early Paleozoic sedimentary and magmatic formations and some related mineral resources. It contains some relics of pre-existing E-W trending structural features composed of early Proterozoie group. The fold belts of the western wing of the Chilienshan-Lüliangshan ε structure which probably began to take shape in Devonian and developed to perfection during Cretaceous times transect the Paleo-Hosi system in the western part and are superposed on it in the central part. The Lungsi system, a brush structure convexing towards the north-east, joins it from the north at its eastern end. The Hosi system consisting of a number of equidistant parallel belts of uplifts and subsidences is transposed upon it. Some of the earlyformed structural features left in the south-western part of this area were involved in the Sikang-Tibetan η system and became modified and distorted. The Paleo-Hosi system and other tectonic "systems said above together with the NNE-NE trending tectonic systems in eastern China seem to suggest a southward movement of the Chinese continental crust.
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