cenozoic造句
61. For Kuqa Basin, there has different subsiding features during its and Cenozoic evolution periods.
62. Liaohe Basin is a fault basin of rift valley type formed in Cenozoic Era.
63. The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
64. Some cenozoic stars like Wusiyuan, Luokaiyuan heep invited to the ribbon - cutting ceremony.
65. The fault activities of Cenozoic have apparent phase and migration.
66. In Mesozoic, the most important interaction occurred between the crust and the mantle, whereas in the older and Cenozoic it did between the lithosphere and the asthenosphere .
67. There are 59 Cenozoic cones, the volcanic texture of which may be classified into cone, dome, lava lake and maar.
68. From late Cretaceous to Paleocene, it is the time of basin extruding, uplifting and denudation, therefore a larger angular unconformity formed between Mesozoic and Cenozoic.
69. The generation of hydrocarbons of the Ordovician source is different from that of Mesozoic nd Cenozoic sources since there were on high plants in the Ordovician Period.
70. The Mesozoic and Cenozoic plutonic intrusive rocks are grouped into the Lhagoi Kangri and Gangdise granite zones.
71. The basin and the mountain were formed by Cenozoic rifting on the basis of the North China peneplain, which was formed in the Late Cretaceous.
72. Taizhong-Jinjiang transverse structure belt is an important Faulted Zone,[www.] which controls the North-South differences of cenozoic diastrophism and current lithosphere movement of Fujian province.
73. The main fracture of the western margin fault zone of the South China Sea is originated from the Mesozoic basement fault, continuously developed into dextral strike-slip fault zone in Cenozoic.
74. From two aspects the authors discuss the influence of Mesozoic and Cenozoic geologic process to the state of regional land resources in the west part of Liaoning Province.
75. Through long terms of tectonic evolutions, it changed into a transform fault in the Cenozoic Era.
76. A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.
77. The deposition velocity of Paleozoic, Mesozoic and Cenozoic assumes unimodal pattern.
78. The new knowledge of the facies indicating significance of foraminifers is the key to the understanding of the Cenozoic paleography of China.
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