藏东丁青蛇绿岩中堆晶辉长岩锆石SIMS U-Pb定年及其意义

刊出日期: 2009-09-15

Zircon SIMS U-Pb dating and its significance of cumulate gabbro from Dengqen ophiolite，eastern Tibet, China

Publish Date: 15 September 2009

摘要: 丁青蛇绿岩位于班公湖-怒江缝合带东段，蛇绿岩的各端元组分出露齐全。纳永拉堆晶辉长岩作为蛇绿岩的端元组分之一，地球化学特征反映可能形成于MOR环境。纳永拉堆晶辉长岩获得SIMS锆石Ｕ-Ｐb年龄为217.8 Ma±1.6Ma。CL照相和测试数据表明，锆石为典型岩浆成因的锆石。锆石定年确定纳永拉堆晶辉长岩形成于晚三叠世，为丁青段班公湖-怒江洋盆的打开时间提供了准确的时间约束。
- 班公湖-怒江缝合带 /
- 藏东丁青地区 /
- 纳永拉堆晶辉长岩 /
- SIMS 锆石U-Pb定年
Abstract: Dengqen ophiolite is located in the eastern of Bangong Co-Nujiang suture zone，and is composed of ultra-mafic rocks, mafic dykes, cumulate gabbro, pillow basalt and siliceous rocks. The geochemical data suggest that the Nayongla cumulate gabbros from Dengqen ophiolite maybe formed under the setting of MOR. Zircons from the cumulate gabbro are all magmatic origin according to their CL images and analytic data. SIMS U-Pb zircon age of 217.8 ± 1.6 Ma is obtained, which suggest that the Nayongla cumulate gabbro formed in Late Triassic. The age of Nayongla cumulate gabbro provides the exact time for the opening of Bangong Co－Nujiang ocean in Dengqen area.
- Bangong Co-Nujiang suture zone /
- Dengqen area /
- eastern Tibet /
- Nayongla cumulate gabbro