B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.

M. Berndt; W. E. Seyfried

B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.

M. Berndt, W. E. Seyfried

Earth and Environmental Sciences-Twin Cities

Research output: Contribution to journal › Article › peer-review

5 Scopus citations

Abstract

Trace elements were determined for 12 celadonite and smectite-rich veins. The oxidative alteration zones have celadonite and Fe-oxyhydroxide and concentrations of K, Rb and B. The non-oxidative zones have Mg-rich smectite (saponite), talc and calcite plus high Li. Apparently, the smectite is enriched with Ni whose source was olivine in the basalt.-K.A.R.

Original language	English (US)
Pages (from-to)	491-497
Number of pages	7
Journal	Initial Reports of the D.S.D.P.
Volume	92
State	Published - Jan 1 1986

Fingerprint Dive into the research topics of 'B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.'. Together they form a unique fingerprint.

Cite this

@article{2100cc26e5394f1d9676ce530552c7eb,

title = "B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.",

abstract = "Trace elements were determined for 12 celadonite and smectite-rich veins. The oxidative alteration zones have celadonite and Fe-oxyhydroxide and concentrations of K, Rb and B. The non-oxidative zones have Mg-rich smectite (saponite), talc and calcite plus high Li. Apparently, the smectite is enriched with Ni whose source was olivine in the basalt.-K.A.R.",

author = "M. Berndt and Seyfried, {W. E.}",

year = "1986",

month = jan,

day = "1",

language = "English (US)",

volume = "92",

pages = "491--497",

journal = "Initial Reports of the D.S.D.P.",

}

TY - JOUR

T1 - B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.

AU - Berndt, M.

AU - Seyfried, W. E.

PY - 1986/1/1

Y1 - 1986/1/1

N2 - Trace elements were determined for 12 celadonite and smectite-rich veins. The oxidative alteration zones have celadonite and Fe-oxyhydroxide and concentrations of K, Rb and B. The non-oxidative zones have Mg-rich smectite (saponite), talc and calcite plus high Li. Apparently, the smectite is enriched with Ni whose source was olivine in the basalt.-K.A.R.

AB - Trace elements were determined for 12 celadonite and smectite-rich veins. The oxidative alteration zones have celadonite and Fe-oxyhydroxide and concentrations of K, Rb and B. The non-oxidative zones have Mg-rich smectite (saponite), talc and calcite plus high Li. Apparently, the smectite is enriched with Ni whose source was olivine in the basalt.-K.A.R.

UR - http://www.scopus.com/inward/record.url?scp=0022860721&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0022860721&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0022860721

VL - 92

SP - 491

EP - 497

JO - Initial Reports of the D.S.D.P.

JF - Initial Reports of the D.S.D.P.

ER -

B, Li, and associated trace element chemistry of alteration minerals, Holes 597 and 597 C.

Abstract

Other files and links

Cite this