| 西藏班戈-切里错地区早白垩世火山岩的时代确定及意义 |
| |
| 引用本文： | 陈玉禄,江元生.西藏班戈-切里错地区早白垩世火山岩的时代确定及意义[J].地质力学学报,2002,8(1):43-49. |
| |
| 作者姓名： | 陈玉禄 江元生 |
| |
| 作者单位： | 四川省地质调查院区调所, 四川双流 610213 |
| |
| 基金项目： | 1∶25万班戈县幅区域地质调查,图幅编号H46C001001 |
| |
| 摘 要： | 对班戈-切里错地区广泛分布的去申拉组中酸性火山岩详细研究认为,去申拉组中酸性火山岩角度不整合于沙木罗组(J3-K1s)之上,被竟柱山组(K2-3j)角度不整合覆盖,同时获126Ma(Rb-Sr)同位素年龄值,证实去申拉组火山岩时代为早白垩世(K1),为同造山期火山岩。去申拉组火山岩的时代确定,并将其从东巧蛇绿岩中分离出来,为蛇绿岩进一步研究提供了依据;为班公错-怒江结合带中段早白垩世造山事件的确定提供了依据。
|
| 关 键 词： | 班公错-怒江结合带 去申拉组 火山岩 同造山期 |
| 文章编号： | 1006-6616(2002)01-0043-07 |
| 收稿时间： | 2001/10/31 0:00:00 |
| 修稿时间： | 2001年10月31 |
AGE AND SIGNIFICANCE OF VOLCANIC ROCK OF EARLY CRETACEOUS IN THE BAN GE-QIELICUO AREAA IN TIBET |
| |
| CHEN Yu-lu and JIANG Yuan-sheng.AGE AND SIGNIFICANCE OF VOLCANIC ROCK OF EARLY CRETACEOUS IN THE BAN GE-QIELICUO AREAA IN TIBET[J].Journal of Geomechanics,2002,8(1):43-49. |
| |
| Authors: | CHEN Yu-lu and JIANG Yuan-sheng |
| |
| Institution: | Regional Geological Surveying Institute of Geological Surveying Academy of Sichuan Province. Shuanglui, Shichuan, 610213, China |
| |
| Abstract: | Our research results show that volcanic rock of Qushenla Formation is angular unconformity with Shamuluo Formation(J3-K1s),and it is covered in angular unconformity by Jingzhuoshang Formation(K1-2j),and its age of Rb-Sr radisotope is 126Ma.All evidence above show that volcanic rock of Qushenla Formation is syntectonic volcanic rock.As time is determined for volcanic rock of Qushenla Formation, it should separate out from Dongqiao ophiolite,it will put out new data for going deep into the research of the ophiolite,and it also should provide the evidence for orogenic event of Early Cretaceous in the Bangongcuo-Nujiang combine zone. |
| |
| Keywords: | Bangongcuo-Nujiang combine zone Qushenla Formation volcanic rock synorogenic period |
| 本文献已被 维普 万方数据 等数据库收录！ |
| 点击此处可从《地质力学学报》浏览原始摘要信息 |
| 点击此处可从《地质力学学报》下载免费的PDF全文 |
