Secondary Ion Mass Spectrometry Bias on Isotope Ratios in Dolomite-Ankerite, Part I: δ18O Matrix Effects-Reference-Cited by-同舟云学术

Secondary Ion Mass Spectrometry Bias on Isotope Ratios in Dolomite-Ankerite, Part I: δ18O Matrix Effects

Author:

Śliwiński Maciej G.¹²,Kitajima Kouki¹²³,Kozdon Reinhard¹⁴,Spicuzza Michael J.¹²,Fournelle John H.²,Denny Adam¹²,Valley John W.¹²³

Affiliation:

1. WiscSIMS; Department of Geoscience; University of Wisconsin-Madison; Madison WI 53706 USA

2. Department of Geoscience; University of Wisconsin-Madison; Madison WI 53706 USA

3. Department of Geoscience; NASA Astrobiology Institute; University of Wisconsin-Madison; Madison WI 53706 USA

4. Department of Marine and Coastal Sciences; Rutgers; The State University of New Jersey; New Brunswick NJ 08901-8521 USA

Funder

U.S. Department of Energy Office of Science

Office of Basic Energy Sciences

U.S. National Science Foundation

NASA Astrobiology Institute

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

Reference52 articles.

3. Absolute 18O content of standard mean ocean water;Baertschi;Earth and Planetary Science Letters,1976

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