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您的检索式：作者名="JosephL.Wooden"
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| 1 | 柴北缘西段花岗岩锆石SHRIMP U-Pb定年及其岩石地球化学特征显示文摘柴北缘西段出露的花岗岩主要有赛什腾山、团鱼山、嗷唠河和三岔沟等岩体,这些岩体的走向为北西向,与区域构造线方向基本一致.岩体的锆石SHRIMP U—Pb定年结果表明,它们的时代从早古生代的奥陶纪到晚古生代的泥盆纪和二叠纪.其中,赛什腾山岩体为(465.4±3.5)Ma,团鱼山岩体两期侵入岩的年龄分别为(469.7±4.6)和(443.5±3.6)Ma;它们均属早古生代奥陶纪;而嗷唠河岩体的石英闪长岩为(372.1±2.6)Ma,属晚古生代泥盆纪;三岔沟岩体也由两期侵入岩组成,其年龄分别为(271.2±1.5)和(260.4±2.3)Ma,属二叠纪.花岗岩的岩石地球化学特征表明,柴北缘早古生代花岗岩具有岛弧或活动大陆边缘花岗岩的属性,原岩可能为中元古代(1.03~1.15Ga)形成的、来源于亏损地幔的拉斑玄武质洋壳,它们的形成与板块的俯冲作用有关;晚古生代花岗岩继承了早古生代花岗岩的特点,其原岩可能为中元古代(1.18—1.29Ga)的岛弧根部下地壳,岩浆物质成分以壳幔混合源为主,它们的形成与造山隆起后不同块体之间的均衡调整有关. | 吴才来 郜源红 吴锁平 陈其龙 JosephL.Wooden FrankK.Mazadab Chris Mattinson | 2008 | 中国科学(D辑)2008，38，8： | 89 |
| 2 | Zircon U-Pb SHRIMP dating of the Yematan batholith in Dulan, North Qaidam, NW China显示文摘The Yematan batholith crops out over 120 km2 in the North Qaidam ultrahigh pressure (UHP) metamorphic belt. It consists of granodiorite, monzogranite and biotite granite and forms an irregular intrusion into Neoproterozoic gneiss that has undergone Caledonian UHP metamorphism. Zircons from the Yematan granodiorite yield a SHRIMP U-Pb age of 397? Ma. These granitic rocks have geochemi- cal characteristics intermediate between I- and S-type gran- ites, and are post-collisional. We suggest that the Yematan granitic rocks were formed during the last exhumation event of the North Qaidam UHP belt. | WUCailai YANGJingsui JosephL.Wooden SHIRendeng CHENSongyong AndersMeibom ChrisMattinson | 2004 | Chinese Science Bulletin2004，49，16： | 14 |
| 3 | Petrogenesis and Dating of Two Types of Granite from North Qilian, China显示文摘Two types of granitic intrusives occur in the lower Paleozoic strata in north Qilian. One is the hornblende- bearing granitic body in Jingzichuan, characterized by the REE total of 90×10-6-106×10-6, LREE/HREE ratio of less than 8 (ranging from 6.9 to 7.8) and zircon SHRIMP age of 464 Ma. These intrusives have island-arc affinity. The other is biotite-bearing granitic body in Huangyanghe with the REE total of 214×10-6-250×10-6, LREE/HREE ratio of more than 8 (ranging from 8.2 to 9.7) and zircon LA-ICP-MS age of 383 Ma. They were tectonically intruded in a post-collisional or within-plate environment. | WUCailai SHIRendeng YANGJingsui YANGHongyi JosephL.WOODEN ZHENGQiuguang CHENGShengyong | 2005 | Acta Geologica Sinica(English Edition)2005，79，2： | 0 |
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