Sediment mineralogy based on visible and near-infrared reflectance spectroscopy-Reference-Cited by-同舟云学术

Sediment mineralogy based on visible and near-infrared reflectance spectroscopy

Published:2006 Issue:1 Volume:267 Page:129-140
ISSN:0305-8719
Container-title:Geological Society, London, Special Publications
language:en
Short-container-title:Geological Society, London, Special Publications

Author:

Jarrard Richard D.¹,Vanden Berg Michael D.²

Affiliation:

1. Department of Geology and Geophysics, University of Utah Salt Lake City, UT 84112, USA

2. Utah Geological Survey, Energy and Minerals Section 1594 W. North Temple, Salt Lake City, UT 84114, USA jarrard@earth.utah.edu

Abstract

AbstractVisible and near-infrared spectroscopy (VNIS) can be used to measure reflectance spectra (wavelength 350–2500 nm) for sediment cores and samples. A local ground-truth calibration of spectral features to mineral percentages is calculated by measuring reflectance spectra for a suite of samples of known mineralogy. This approach has been tested on powders, core plugs and split cores, and we conclude that it works well on all three, unless pore water is present. Initial VNIS studies have concentrated on determination of relative proportions of carbonate, opal, smectite and illite in equatorial Pacific sediments. Shipboard VNIS-based determination of these four components was demonstrated on Ocean Drilling Program Leg 199.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

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