mesozoic造句
61, Baixiangshan iron deposit is located in the southern part of Ningwu Mesozoic faulted basin. It is classified as Fenghuangshan-type iron deposit in the model of Ningwu porphyritic type iron deposit.
62, Typical columnar joint structure of considerably large scale found in recent years is distributed in various localities in Mesozoic acidic volcanic rocks in Zhejiang.
63, Many collisions of considerable size and periods of supervolcanism occurred early in the Mesozoic era.
64, The high frequency part of Dongsha high-value magnetic anomaly may be related with Cenozoic basalt and Mesozoic magmatic rocks, and the low frequency part developing high-velocity lower crust.
65, The Phanerozoic is divided into three eras — starting with the earliest, these are the Paleozoic, Mesozoic, and Cenozoic.
66, Mesozoic intrusive complex in central eastern North China Block (NCB) is mainly composed of two sets of rock associations such as appinite and granodiorite.
67, The earlier-stage mineralization was intensely superposed by the tectono-magmatic thermal fluid of the later Mesozoic in the middle part of the Fujian Province.
68, There are 5 kinds of geological settings: metamorphic basement area, geosyncline area, cover area, Mesozoic volcanic fault basin and tectonic magmatic active belts.
69, The southern region includes western and southeastern Yunnan as well as western and southern Guangxi. The Late Palaeozoic and Early Mesozoic radiolarian chert sequences occur there.
70, There are recognizant divergences on the Mesozoic tectonic evolution of south China, which is to a certain extent related to inadequacy of integrated study on multiple geological elements.
71, Iron ores in the Gushan deposit, Anhui Province, occur in a contact tone between Mesozoic gabbro diorite and its country rocks dominated by Triassic shale, siltstone and sandstone.
72, The Shixi Formation which rests unconformably on the Ehulin Formation and is unconformably overlain by the Zhoujiadian Formation is the upper part of the Mesozoic volcanic-sedimentary strata.
73, The Mesozoic granitic volcanic - intrusive complexes are widely dispersed over the eastern Guangdong area.
74, 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 .
75, Multichannel seismic reflection, magnetism and drilling data show that there are Mesozoic strata in the East China Sea (ECS) shelf basin.
76, As the dominator of the Mesozoic, it is the focus of the science.
77, It was in the upper Trias of Mesozoic approximately 180 million years ago and Shanghai and South Jiangsu were ancient continents then.
78, Large scale granitic magma during Mesozoic was the major carrier for gold.
79, Pterosaur bones have similar features, as do those of several other groups of Mesozoic reptiles.
80, 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.
81, 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.
82, I-type granites, aplites and pegmatites outcropping in Mesozoic metamorphic belt of the southeastern coast of Fujian Province contain commonly magmatic garnets and primary muscovites .
83, The Late Mesozoic characterized by higher temperature gradient is main period of gas generation and migration of Paleozoic coal series and carbonates.
84, The Mesozoic and Cenozoic plutonic intrusive rocks are grouped into the Lhagoi Kangri and Gangdise granite zones.
85, This study use the microcosmic methods to analyze the micro- fabrics of the Mesozoic and Neozoic chert formations and the Modern sinters in southern Tibet, try to reveal their geological information.
86, The exhalation-spout type deposits of the early Paleozoic era and the orogenic type deposits of the late Paleozoic to early Mesozoic era are the most important deposit groups.
87, Songliao Basin is a expanding and rifted basin which was formed in Mesozoic era.
88, The Songliao Basin is a largescale petroliferous extensional sedimentary basin in Late Mesozoic.
89, The main driving forces of petroleum migration in the Mesozoic are buoyancy and abnormal pressure.
90, Since primitive society, the people the reason that can mesozoic save down in the so bad natural environment, is based on the clan member interior close cooperation.
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