The Research Advances in the Rutile in the Subduction-Collision Zone, High Pressure and Ultrahigh Pressure Metanorphic Zone

doi:10.11867/j.issn.1001-8166.2006.01.0047

Advances in Earth Science ›› 2006, Vol. 21 ›› Issue (1): 47-52. doi: 10.11867/j.issn.1001-8166.2006.01.0047

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The Research Advances in the Rutile in the Subduction-Collision Zone, High Pressure and Ultrahigh Pressure Metanorphic Zone

Yu Jinjie ¹,Wang Denghong ¹,Wang Pingan ²,Xu Jue ¹,Li Xiaofeng ¹,Chen Yuchuan ³,Chen Zhenyu ¹

1.Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;2.Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;3.Chinese Academy of Geological Sciences, Beijing 100037, China

Received:2005-08-18 Revised:2005-11-01 Online:2006-01-15 Published:2006-01-15

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Yu Jinjie,Wang Denghong,Wang Pingan,Xu Jue,Li Xiaofeng,Chen Yuchuan,Chen Zhenyu. The Research Advances in the Rutile in the Subduction-Collision Zone, High Pressure and Ultrahigh Pressure Metanorphic Zone[J]. Advances in Earth Science, 2006, 21(1): 47-52.

Rutile is a widely distributed mineral in high-grade metamorphic rocks and hydrothermal deposits. The rutile studies of the subduction-collision zones and high pressure and ultrahigh pressure metamorphic zones include (1) role of the rutile in the subduction-collision zone; (2) polymorph of rutile; (3) U-Pb dating of rutile and (4) tracing of rutile for a source rock. These studies is very important not only for origin and characteristics of the akadite in the subduction-collision zone but also for the depth, temperature and pressure of continental ultra-deep subduction, and age of the metamorphic event in high-grade metamorphic terrane, and tracing of the rutile-hosted source rock.

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