2017
DOI: 10.1016/j.gca.2017.04.036
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Raman spectral, elemental, crystallinity, and oxygen-isotope variations in conodont apatite during diagenesis

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Cited by 33 publications
(36 citation statements)
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“…This B‐type carbonate substitution for PO 4 3− with associated vacancy formation and lattice distortion only leads to a comparably small spectral shift . However, the combination with the minor A‐type substitution (B:A ≈9:1) can then account for the observed correlated variation in Γ and ν due to structural disorder associated with the substitution as has been shown in several geological and biomineral apatite systems …”
Section: Discussionmentioning
confidence: 75%
“…This B‐type carbonate substitution for PO 4 3− with associated vacancy formation and lattice distortion only leads to a comparably small spectral shift . However, the combination with the minor A‐type substitution (B:A ≈9:1) can then account for the observed correlated variation in Γ and ν due to structural disorder associated with the substitution as has been shown in several geological and biomineral apatite systems …”
Section: Discussionmentioning
confidence: 75%
“…; Katvala & Henderson ; Zhang et al . ) largely reflect the variety of diagenesis of the skeletal tissue influenced by hydrothermal or meteoric alteration and other types of remineralization.…”
Section: Discussionmentioning
confidence: 99%
“…Raman spectroscopy is a powerful, fast, and nondestructive experimental technique, which has been extensively applied not only in basic scientific researches, but also for practical applications. It can provide physical, chemical, and structural characteristics of investigated samples [11][12][13][14][15][16][17][18][19][20][21][22][23][24]. In the past decade, Raman spectroscopy has been applied for quantitative and qualitative studies of various types of minerals.…”
Section: Introductionmentioning
confidence: 99%