Basal lherzolites in the Bay of Island ophiolite: origin by detachment-related 
telescoping of a ridge-parallel melting gradient

Suhr, G.; Batanova, V.

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Basal lherzolites in the Bay of Island ophiolite: origin by detachment-related telescoping of a ridge-parallel melting gradient

Suhr, G., & Batanova, V. (1998). Basal lherzolites in the Bay of Island ophiolite: origin by detachment-related telescoping of a ridge-parallel melting gradient. Terra Nova, 10, 1-5.

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Item Permalink: https://hdl.handle.net/11858/00-001M-0000-0014-97FE-7 Version Permalink: https://hdl.handle.net/11858/00-001M-0000-0014-97FF-5

Genre: Journal Article

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Creators:
Suhr, G.¹, Author
Batanova, V., Author

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1Geochemistry, Max Planck Institute for Chemistry, Max Planck Society, ou_1826288

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Dates: Date issued: 1998

Publication Status: Issued

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Rev. Type: Internal

Identifiers: eDoc: 373542
Other: 4059

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Title: Terra Nova

Source Genre: Journal

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Pages: - Volume / Issue: 10 Sequence Number: - Start / End Page: 1 - 5 Identifier: -