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构造气候
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  tectonic-climatic
     They coincide with the 0.4 Ma and 1.2 Ma tectonic-climatic sub-cycle since 8.0 Ma B.P.
     P . 以来的构造气候旋回 ,亚旋回的准 1.2Ma及 0 .4Ma周期相一致。
短句来源
  “构造气候”译为未确定词的双语例句
     ON TECTONOCLIMATIC CYCLE OF QUASI PERIOD OF 1 2Ma IN LATE CENOZOIC
     关于晚新生代准1.2Ma周期构造气候旋回
短句来源
     The boundaries of tectonoclimatic cycles determined from the stratigraphic records in the Loess Plateau giving solar calendar ages of 0. 07, 0. 46, 0. 83, 1. 32, 1. 70, 2. 08, 2. 47MaBP respectively correspond to the time intervals where there is a decrease of the eccentricity of the Earth's orbit.
     据黄土高原地层记录划分的构造气候旋回界限,日历年龄分别为0.07、0.46、0.83、1.32、1.70、2.08、2.74MaBP,对应于偏心率曲线波动幅度由大变小时段的特定转折位置。
短句来源
     VOLCANIC ACTIVITIES AND TECTONIC-CLIMATIC CYCLES
     火山活动与构造气候旋回
短句来源
     TECTONIC CLIMATE RESPONSE IN THE GEOMORPHOLOGY OF THE WEIHE RIVER VALLEY AROUND BAOJI,SHAANXI PROVINCE
     渭河宝鸡段河谷地貌的构造气候响应
短句来源
     The forming of sequence boundaries, which can be divided into two types according to the genetic mechanism: tectonic controlling boundary (type T) and tectonic-climate synthetical controlling boundary (type TC) in Jiyang depression, is controlled by climate and tectonic movement.
     断陷湖盆中层序界面按成因机制可分为构造型(T型)和构造气候综合型(TC型),T型界面一般对应于三级层序界面,TC型界面一般对应于二级或一级层序界面。
短句来源
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  相似匹配句对
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
短句来源
     The X.
     在构造 X.
短句来源
     VOLCANIC ACTIVITIES AND TECTONIC-CLIMATIC CYCLES
     火山活动与构造气候旋回
短句来源
     TECTONIC AND CLIMATIC ELEMENT-CONTRLLED EVOLUTION OF THE YALUNGZANGBU RIVER IN SOUTHERN TIBET
     在构造气候因素制约下的雅鲁藏布江的演化
短句来源
     Atmosphere and Climate
     大气层和气候
短句来源
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  tectonic-climatic
This uplifting is perhaps the driving force of the tremendous environmental change of tectonic-climatic circulation at the break of the early and middle Pleistocene in China.
      


Various microfacies in different depoeitional systems have been recognized through the study of moderndeposits in Xingyun lake basin. Cenozoic sediments revealed by exploration drilling are subdivided into threefacies associations, namely (1) alluvial fan-flooded plain-swamp peatbog, (2) shallow lake-alluvial fan and(3) lacustrine plain-shallow lake. Tectonic and climate control on sedimentation and development of thelake basin and its implication to petroleum geology is also discussed.

本文通过对江川盆地和星云湖现代沉积作用的研究,划分了湖周围晚新生代沉积的三种相组合,并讨论了构造、气候对沉积作用的控制和盆地发育特点及其在石油地质方面的启示。

A set of coal-bearing formation inluding very thick brown,oal beds and dominant macroclastic rock is developed within the narrow-long intermountain basic in Zhenan, Longlin, Yunnan. It looks like the river swamp deposit in appearance, and adispute arises. On the basis of re- search and analysis on the structare, paleoclimate, paleobotany, paleohy- drologic condition and paleogeographic environment during the period of coal formation in this region, it is considered that the macroclastic materials will be the...

A set of coal-bearing formation inluding very thick brown,oal beds and dominant macroclastic rock is developed within the narrow-long intermountain basic in Zhenan, Longlin, Yunnan. It looks like the river swamp deposit in appearance, and adispute arises. On the basis of re- search and analysis on the structare, paleoclimate, paleobotany, paleohy- drologic condition and paleogeographic environment during the period of coal formation in this region, it is considered that the macroclastic materials will be the deposit of alluvial fan with front margins one upon another into lake instead of the river swamp as is often said. It is a special fan-lake environment of coal formation. Seeing that the basin is small, the differentiation of coaly facies is not obvious and the tran- sportation distance is short, the macroclastic rock will become the main sediment in the lake swamp. Such a coal formation environment is dif- ferent from those in delta plain and coves between fans at home and abroad.

在云南龙陵镇安狭长的山间盆地内,发育着一套以粗碎屑岩为主并含巨厚褐煤层的含煤建造,外表根像河流成煤环境,为此颇有争议。本文通过对该区成煤期构造、气候、植物、水文条件及其地理环境的研究分析,认为此粗屑物质并非通常所说的河流沉积物,是大量边缘互相重量入湖的冲积扇沉积,是个特殊的扇湖成煤环境。由于盆地小,相分异差,搬运短,含煤建造和湖沼是以粗碎屑岩为主。故它不同于国内外一般扇间湾和扇三角洲平原成煤。

This paper tries to investigate the formation process of Nantai island in Fuzhou by the regional analysis of geological structure, hydrological condition and historicail factors. It shows that Nantai island has once existed in several small rock islands which fiery are tied in a large island composed of half rock and half sahd.

本文应用区域分析的方法,着重从地质构造、气候和水文状况、历史因素三方面分析了福州南台岛由一个面积较小的岩石岛,演变为一个面积较大的半岩半沙的岛连岛的发展过程。

 
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