| 雪峰山西侧地带的地洼型造山-造盆作用 |
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| 引用本文： | 王伏泉,梁新权.雪峰山西侧地带的地洼型造山-造盆作用[J].大地构造与成矿学,2002,26(2):121-125. |
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| 作者姓名： | 王伏泉 梁新权 |
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| 作者单位： | 中国科学院长沙大地构造研究所,湖南,长沙,410013 |
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| 基金项目： | 中国科学院重大项目，KZ-95-2-J1-007， |
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| 摘 要： | 在晚三叠世前长期处于地台体制的雪峰山西侧地带,上三叠统和中-新生界的沉积相、物质成分、构造变动和地台构造层的构造变动反映,这里于地洼阶段发生了强烈的造山-造盆作用,造成了当今海拔反差达约千米的盆、山景观。这类地洼型造山-造盆作用具有多种运动方式。
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| 关 键 词： | 地洼 雪峰山西侧地带 造山-造盆 |
| 文章编号： | 1001-1552(2002)02-121-05 |
| 修稿时间： | 2001年8月20日 |
THE OROGENY AND BASIN-FORMING PROCESS OF WESTERN XUEFENGSHAN MOUNTAINS, HUNAN PROVINCE, CHINA |
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| Abstract: | In the area of the west side of the Xuefengshan mountains there occurred a p latform system for a long time before late Triassic.The s edimentation facies,material comp osition and structural event of the upper Triassic and Meso-Cenozoic,a nd the platform structural layer indicate that an intense orogeny-basin-making process had happened in diwa (depression)stage in this area.As a result,there appears a land-scape of basin and mountain,and their hight deviation is about up to 1000m .Obviously,the oroge-ny-basin-making process of the type of diwa (depression)has various patterns of movement. |
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| Keywords: | Diwa (depression) western Xuefengshan mountains orogeny-basin-forming process |
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