倒转向斜
![d3 向斜 背斜](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A73F17AD8D15768C79A14F5C9CB0DD5719669598CD5136A142FF05ADE69F4317869DB15BB1A50900C44D9B506F00A71DEF7D2EBC159556126FCD5FE17C7902FCC5DA1885893097AE7E59CD98627A5C80407)
d3 向斜 背斜
图片尺寸1080x810![背斜成谷,向斜成山示意](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9DE1BF9EE10DA4F2FBF1A38A64817EB708D982C91E24A8B7A86109E707A967663D0C992CC1E035262224A4F81554B44A862E0B6E2455B25FE19AB568377A9B34EC49FAB70093614137524895ADE65360A)
背斜成谷,向斜成山示意
图片尺寸1080x810![背斜和向斜的判断](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9F42668E54F5E835E69DD8761C4D4252930733024119F2876D01DF896FB89D8F68E9D309826FE3A42493F8AFE21D02916365DFF3CB5B752C3676FBCF5679E1437107D9D3115849DB3BA261AE543D41181)
背斜和向斜的判断
图片尺寸1080x810![一图搞懂背斜和向斜](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A730EF94A59487E78F5C66F2EBE2BE7F40B918857D6A17118FE9DA6A806AF32A62725A83F3389BBD33AC7F4DEC800AE52369BF9C6988A959D83C5EF8DA275BEA29A9448C3E897261A8ED4596F9B6336A318)
一图搞懂背斜和向斜
图片尺寸961x1280![新 4 老 背斜 4 向斜 4 褶皱——岩层受到强烈碰撞](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E8392C38225AB10A66599D522B9CE0409F2A82E496CED9D6355F53EFE009F90A184DCBE4E5E0CE16E347449AE57B8686B85B80C84D8DC3DF1CEE3DFC45334BF5FD9D8E37D37D5D5617ED688D1DB35A67409)
新 4 老 背斜 4 向斜 4 褶皱——岩层受到强烈碰撞
图片尺寸1080x810![如何确定一张图里的褶皱地形是背斜还是向斜](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A733AD5D705F377B85536BFFD4BC5505FFCD3FA3D4932821B200B10AFFEA67A40C760CBBF29EC68B74293158A6EB40D3FC4DF259F56A62AD88B4B635D7BC12D800543F36EDC19EF12C50F5D0C6500271E33)
如何确定一张图里的褶皱地形是背斜还是向斜
图片尺寸435x298![趣味地理——背斜,向斜,地形倒置现象](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9C447168707784BCB50784750DF9246504757BA1965B29F53EE9676B35B94DB65086A516DDFE3F97D5B3F10190BB6DD237E9E93BF3B5D7621E7CEA6681730A3BA8A6465B83B5853603FDBF65D8F7BD536)
趣味地理——背斜,向斜,地形倒置现象
图片尺寸640x400![地理小常识:怎么避免对背斜和向斜的错误认识!](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E832CB9DB5CC81F1E58ACD96413F9D41CB556D3CCFB86060181C67D33C0D70E7B005398E43CBA8475F7800BA7CBE923AFCB4BB4E5073D7CE1AF6A1368EDAB664067F3C92D1F391932D3C3C89E804E75F5D4)
地理小常识:怎么避免对背斜和向斜的错误认识!
图片尺寸500x351![高中地理——山的形成(向斜,背斜)](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A734369B52EA74703E90E0CD27B019F7629B493FF5F0D0973BDF707A62EAF8D608307758867716A9A065C72E3BB925A0F33FF6B0BE927455F0CE77261FE628E46FBDDF904F0A7A1B0B7CB902F4886F656B8)
高中地理——山的形成(向斜,背斜)
图片尺寸640x237![判断向斜背斜的最主要因素是什么? - 知乎](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A7307224C22CBC07009E19DC0AB98561DBC509EA68B38E283616937740D7C167E610A5CCA6E5CC84FC7A66701FCBE876C590CBF26264A440C1AE3E953D07A7DE8E332F7C094247ACC9FCD7955D4D39F9FC0)
判断向斜背斜的最主要因素是什么? - 知乎
图片尺寸1633x834![3 褶皱ppt 工程地质 向斜 一般岩层向下弯曲,两侧岩层向内倾斜,核部](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9921C476D87914D459D64A6E8805FBEF12A954C5728544BF608CE7436B88F5A48BF5F5C582104B880B47D4D59CA0290CD12A4807DB974D99A54159F1DACA1BEAAEB653F3ABF5D9272A80701320DCAF133)
3 褶皱ppt 工程地质 向斜 一般岩层向下弯曲,两侧岩层向内倾斜,核部
图片尺寸1080x810![向斜两边物质疏松易被侵蚀,但槽部物质结构紧密不易被侵蚀,就会形成](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A73D8CA0DD3ED70A664D606567EB7C2E9F8D1948A8A73ADE37FCF796C5BCC556F6AFE1EE84BF75DD3D067979872D2D8BFF410F16FD1DE9DF4F9C5061E07FB125D8FF1C069A1434CA12D6F61E5703ADD00B2)
向斜两边物质疏松易被侵蚀,但槽部物质结构紧密不易被侵蚀,就会形成
图片尺寸640x252![在侧向作用力下发生弯曲称为褶皱,岩层向上凸起为背斜,向下凹入为向斜](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E938F8C5AC242489B08D9BFD0D5FB98094B33E5A937D98AF3938439FD8CF15CE572B5D2F87B05928F52F3A3258C6261FD668434EE1D92C878C240109186213C8ED1438DFEC2F246A8C422AD17AB0234A4F)
在侧向作用力下发生弯曲称为褶皱,岩层向上凸起为背斜,向下凹入为向斜
图片尺寸1041x481![第2节山岳的形成](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A731DD7F619C63E3087FAC0F678CD953D8CD7A644948A9FFB119EBA9F52D023E617EE1D0EE4DCFE1BA304F370B751D7B285130CD541761A7EC109D7BA908AD804D125BA084F8547555D7AB6C100A7CCEF2A)
第2节山岳的形成
图片尺寸475x177![向斜与背斜的成因](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A736C35567952C31D9080543EEA45BCCEE4A4B18E083903BF38F346154D07CF4D2EA3B699EE5E5FBEE7CE296FAD02EBC63C7526DBCC8D9FAA3785AFE87351F7F49D38E447997E847F34477D346E96F7DF9C)
向斜与背斜的成因
图片尺寸512x768![背斜横截面中间岩层老,两侧新(上新下老,凸新则老);向斜横截面中间](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E906F4BA89C60D236DE17B426F118A338EF4B036E9B969D5FFEF252394ADDB4A32909020D613DFF21274B8A4582704842638371C4C2B3E81E88705926530DAFE0CC796EF570DFC3158D1CB71B4416F35ED)
背斜横截面中间岩层老,两侧新(上新下老,凸新则老);向斜横截面中间
图片尺寸1220x327![向斜](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E835083D1B717A9FF1A1CA6056B3E5BF6BA45E46E689483C9EA41F63D749267A18BDC226622F781E74BD949708951B7F087F4FC6FF75BDA65EDF196F58B4720F52AA4DEC0D598863651518DDD5130BAB2CE)
向斜
图片尺寸1080x810![图中有2个背斜,2个向斜.](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A73BC7BCD30EA5FE69FFBE63F1B471E7A0FA3D50AC87B6B2523116A67A67FA8ED59E90EAC6D170ED44B6D03C3092F4570EBC14938980A8C04AA347F41C0FBD4BD3F89C7F69BB9382F0396F9438FB8BB7EB5)
图中有2个背斜,2个向斜.
图片尺寸566x334![图7 背斜(a)与向斜(b)回转弯之另一例, 其中两者的共同翼c发生倒转](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9B01499F059072D0CA9C3446CCB08E1CEF279A37456303F8179BDD5E035AFC09714B17EC39E085339F89622A78F5A1093991FBD20CA244ECAE89E7ABB765D3813BC006C1DFFC914D4F1F6FB5F98417FB8)
图7 背斜(a)与向斜(b)回转弯之另一例, 其中两者的共同翼c发生倒转
图片尺寸1273x676![后来由于外力作用的影响,即背斜顶部物质疏松受侵蚀形成谷地,向斜两翼](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E830ECC917CCE9E3B13EC4E04BD735092AB7E0CFD55A47223953501C96FD5DC71DFF0B0E863C998133808D3AD1730CAE9B204FFA30C741C1360570F8570CFDBEA41D10AC45210C938DCD9463B81D07A9292)
后来由于外力作用的影响,即背斜顶部物质疏松受侵蚀形成谷地,向斜两翼
图片尺寸479x322