@misc{vandenberg2006ttmo, author={Michael D {Vanden Berg} and Richard D {Jarrard}}, title={{(Table T1) Mineralogy of ODP Leg 199 and DSDP Hole 16-162 sediments - comparison of methods}}, year={2006}, doi={10.1594/PANGAEA.776949}, url={https://doi.org/10.1594/PANGAEA.776949}, note={Supplement to: Vanden Berg, MD; Jarrard, RD (2006): Data report: High-resolution mineralogy for Leg 199 based on reflectance spectroscopy and physical properties. In: Wilson, PA; Lyle, M; Firth, JV (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 199, 1-23, https://doi.org/10.2973/odp.proc.sr.199.203.2006}, abstract={During Ocean Drilling Program Leg 199 in the equatorial Pacific, visible and near-infrared spectroscopy (VNIS) was used to measure the reflectance spectra (350-2500 nm) of 1343 sediment samples. Reflectance spectra were also measured for a suite of 60 samples of known mineralogy, thereby providing a local ground-truth calibration of spectral features to percentages of calcite, opal, smectite, and illite. The associated algorithm was used to calculate mineral percentages from the 1343 spectra. Using multiple regression and VNIS mineralogy, multisensor track physical properties and light spectroscopy data were then converted into continuous high-resolution mineralogy logs.}, type={data set}, publisher={PANGAEA} }