One possible origin of olivine in Copernicus crater: the remnants of projectile

来源 :International Symposium & Summer School on Planetary Science | 被引量 : 0次 | 上传用户：rsdt25302530

【摘要】

：

【作者】

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Z.Yue B.C.Johnson D.A.Minton H.J.Melosh K.Di W.Hu Y.Liu

【机构】

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State Key Laboratory of Remote Sensing Science,Institute of Remote Sensing and Digital Earth,Chinese

【出处】

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International Symposium & Summer School on Planetary Science

【发表日期】

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2013年4期

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　　The mineral olivine has been found in the central peaks of Copernicus crater and usually interpreted as excavated from deep lunar crust or even mantle.In the paper we studied the formation of Copernicus crater through hydrocode simulation and proposed that the olivine was more possible from the projectile remnant than from the deep.

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One possible origin of olivine in Copernicus crater: the remnants of projectile

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