Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont PDF Download

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Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont

Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont PDF Author: N. K. Foley
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 40

Book Description
A study of Pb-Zn-Cu mineralization resulting from syngenetic sedimentary-exhalative and diagenetic replacement processes in structures in carbonate and silciclastic platform rocks of Cambrian and Ordovician age that form the lowlands between the Green Mountain massif and the Adirondack massif in western Vermont.

Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont

Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont PDF Author: N. K. Foley
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 40

Book Description
A study of Pb-Zn-Cu mineralization resulting from syngenetic sedimentary-exhalative and diagenetic replacement processes in structures in carbonate and silciclastic platform rocks of Cambrian and Ordovician age that form the lowlands between the Green Mountain massif and the Adirondack massif in western Vermont.

Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont

Geologic, Geochemical, and Isotopic Studies of a Carbonate- and Siliciclastic-hosted Pb-Zn Deposit at Lion Hill, Vermont PDF Author: Geological Survey (É.-U.)
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 0

Book Description
A study of Pb-Zn-Cu mineralization resulting from syngenetic sedimentary-exhalative and diagenetic replacement processes in structures in carbonate and siliciclastic platform rocks of Cambrian and Ordivician age that form the lowlands between the Green Mountain massif and the Adirondack massif in Western Vermont.

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