Yu. K. Burlin. THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(2): 150-153.
Citation:
Yu. K. Burlin. THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(2): 150-153.
Yu. K. Burlin. THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(2): 150-153.
Citation:
Yu. K. Burlin. THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(2): 150-153.
THE INSTABLE ZONES IN DIFFERENT LITHOFACIES OF SEQUENCE AND PROPERTY CHANGES OF THE ROCKS
The reasons of basin's formation are:unsteady states of substance in deep zones of tectono-sphere,increasing of asthenosphere thickness and decreasing of the crust thickness consequent-ly. There are some levels of energetic instability in most of sedimentary basins. It reflects in nonlinear exchanging of properties of the rocks.
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