1) NAPPE TECTONICS IN ANHUI
安徽的推覆构造
2) nappe structure
推覆构造
1.
A discussion on nappe structure pattern in the jiu mountains and the south of the lower reaches of the changjiang river by the remote sensing image;
根据遥感影像讨论九岭──江南地区的推覆构造格局
2.
Latest Permian-earliest Triassic nappe structure in the Ulan Haya area on the northern margin of the North China platform;
华北地台北缘乌兰哈雅地区二叠纪末—三叠纪初推覆构造
3.
Discovery and significance of nappe structure in Yucheng area.
禹城地区推覆构造的发现及意义
3) nappe
[英][næp] [美][næp]
推覆构造
1.
On the basis of analysing the structural features and the genetic mechanism of nappe, gliding nappe and fault-block structures in Linru Coalfield, Hexichen, Wenquan Street and the deep part of Chaochuan mining area are considered as the favourable districts for tracing coal.
在分析临汝煤田的推覆构造、滑覆构造及断块构造特征和成因机制的基础上,指出了河西陈、温泉街、朝川矿区深部等找煤的有利区段。
2.
The comprehensive analyses from strata distribution,gravity,geomagnetism,seismic and CEMP data show that the thrust structural belt in western margin of Ordos basin is composed of Liupanshan arc thrust system and Zhuozishan-Helanshan thrust system,which are two independent nappe tectonic systems.
地层分布、重力、磁力、地震、CEMP多种资料综合分析认为,鄂尔多斯盆地西缘冲断构造带由六盘山弧形冲断体系和桌子山-贺兰山冲断体系组成,它们是互为独立的冲断推覆构造;明确指出,六盘山弧形冲断体系为祁连地体拼贴到华北陆缘地体(鄂尔多斯地块西部)之上的冲断推覆构造,具有独特的双层地体叠置结构。
4) thrust
[英][θrʌst] [美][θrʌst]
推覆构造
1.
The northern Qinling margin thrust structural zone in S→N direction is composed of two structural zones which are Yiyang-Lushan fault zone and Xiong er rock sheet.
主要包括秦岭北缘反冲推覆构造带，以宜阳-鲁山断裂带和熊耳岩片为主体，由S→N逆冲推覆，栾川-伏牛山推覆构造带特征典型，分带性强，由N→S推覆；马超营走滑转换构造带位于二者之间，为一正花状构造带。
2.
In the Huaqiao-Dajiangkou area, there are developed a series of imbricated thrust nappes on the foreland faulted belt northwest of the collision zone between the northwestern and central Hunan terrains.
湘西北地体与湘中地体碰撞拼贴带北西侧的前陆冲折带上发育一系列叠瓦状排列的逆冲推覆构造 ,向北西方向推覆 ,具双重逆冲推覆特征。
5) nappe tectonics
推覆构造
1.
Nappe tectonics was classified into three types thrust nappe tectonics, slipping tectonics (stretch nappe tectonics) and tenacity nappe tectonics.
依据推覆构造形成的力学机制，将推覆构造分为边冲推覆构造、滑覆构造和韧性推覆构造三大类型。
6) thrust nappe structure
推覆构造
1.
The nappe structures in the area are formed in the late Cretaceous and may be divided into 4 deformable zones,namely,imbricated thrust nappe structure zone,closed folded-thrust faulted deformable zone,wide-gentle folded-faulted turned folded zone and decollement folded-faul.
它主要由韧性剪切带、韧脆性剪切带和推覆构造等构成。
2.
The North Wuyi area is characterized by advantageous mineralizing geological conditions and widespread mineral resources, but the formation and conservation of ore deposits are mainly controlled by thrust nappe structure.
北武夷地区成矿地质条件优越,矿产资源分布广泛,而广泛发育的推覆构造深刻影响着矿床的成生与保存。
补充资料：安徽
安徽概况安徽省名取安庆、徽州二府名字第一个字组合而成，面积１３.９６万平方公里。省会合肥。安徽气候安徽省淮北为暖温带湿润季风气候，淮河以南为亚热带湿润季风气候，四季分明为其主要特征。年平均气温１６摄氏度，一月份１－４摄氏度，零摄氏度等温线基本上与淮河干流吻合：七月在２９摄左右。全年无霜期２００－２５０天。年平均降水量，淮北７００－８００毫米，南部一般８００－１７００毫米，大别山，黄山多雨中心，黄山的降水量高达２０００毫米以上。１９６９年７月１４日霍山降水量２８７.７毫米，为本省最大日降水量。淮北的降水年变率大，夏季集中，易出现春旱丰涝，江南则为梅雨区，夏季可发生伏旱。安徽经济安徽农业具有南北过渡特征。淮北以小麦杂粮为主，已发展成商品粮、生猪生产基地。长江淮河间为鱼米之乡，作物以水稻、油菜为主。淮河流域芝麻、烟叶，沿江和淮北棉花，及各地山区茶竹林特产，长江、巢湖鱼虾也很重要。本省两淮煤矿是华东地区重要能源基地，马鞍山钢铁、铜陵有色冶金在全国居重要地位。淮南、合肥矿山机械，蚌埠水利机械、淮南煤化工、造纸、安庆石化，合肥、安庆、芜湖等地的纺织、食品，及屯溪制茶、蚌埠卷烟等工业也很有名气。传统手工业名优产品有泾县宣纸、毛笔和歙县墨砚。水陆交通便利，皖南、淮北、合九的铁路和淮河流域内河航道迅速发展。沿江有安庆、芜湖、裕溪口等河港。安徽旅游风景名胜有以奇松、怪石著称的黄山，佛教名山九华山，以及天柱山、琅琊山。合肥三国古战场逍遥律、马鞍山采石矶、亳州华佗庵等也很有名。
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