2016•Dizhi tongbaoRequires access

Petrological and petrochemical characteristics and geological significance of Yueyas- han ophiolite

Liao Yunfeng, HU Xinzhuo, Haifeng Cheng, Xuming Xu

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Abstract

Yueyashan ophiolite is located in the Hongliuhe-Xichangjing ophiolite belt in the eastern part of Yueyashan area. Yueyas?han ophiolite suite is exposed fairly completely, consisting in upward succession of ultrabasic complex, gabbro, layered basalt and pil?low basalt as well as radiolarian siliceous rocks. Petrological, petrochemical and geochemical data show that the main unit in the ophi?olite suite originated from mantle source and it is very similar to the modern oceanic crust ophiolite. The plagioclase granite associat?ed with ophiolite unit belongs to mantle type oceanic plagioclase granite;in addition, it is a part of the ophiolite. Gabbro and basalt were both formed in a normal mid-ocean ridge (N-MORB) environment.

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What this paper is about

Yueyashan ophiolite is located in the Hongliuhe-Xichangjing ophiolite belt in the eastern part of Yueyashan area. Yueyas?han ophiolite suite is exposed fairly completely, consisting in upward succession of ultrabasic complex, gabbro, layered basalt and pil?low basalt as well as radiolarian siliceous rocks. Petrological, petrochemical and geochemical data show that the main unit in the ophi?olite suite originated from mantle source and it is very similar to the modern oceanic crust ophiolite. The plagioclase granite associat?ed with ophiolite unit belongs to mantle type oceanic plagioclase granite;in addition, it is a part of the ophiolite. Gabbro and basalt were both formed in a normal mid-ocean ridge (N-MORB) environment.

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Available abstract

Yueyashan ophiolite is located in the Hongliuhe-Xichangjing ophiolite belt in the eastern part of Yueyashan area. Yueyas?han ophiolite suite is exposed fairly completely, consisting in upward succession of ultrabasic complex, gabbro, layered basalt and pil?low basalt as well as radiolarian siliceous rocks. Petrological, petrochemical and geochemical data show that the main unit in the ophi?olite suite originated from mantle source and it is very similar to the modern oceanic crust ophiolite. The plagioclase granite associat?ed with ophiolite unit belongs to mantle type oceanic plagioclase granite;in addition, it is a part of the ophiolite. Gabbro and basalt were both formed in a normal mid-ocean ridge (N-MORB) environment.

Key concepts: Ophiolite, Gabbro, Geology, Geochemistry, Basalt, Pillow lava, Ultramafic rock, Oceanic crust

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