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Virginia Polytechnic Institute and State University

The crystal chemistry of titanite

Abstract

dc:description.abstract

The chemical substitutions of primary importance in natural titanites are (Al,Fe)<sup>3+</sup> + (F,OH)<sup>-</sup> ⇆ T<sub>1</sub><sup>4+</sup> + O<sup>2-</sup> , where total Al + Fe is not greater than 30 mol % and Al is usually predominant. Electron microprobe analyses and bond strength considerations suggest that Al prefers the octahedral site in natural titanites, whereas ubiquitous rare earths substitute for Ca. Ion microprobe mass analysis indicate that Pb, U, and Th are present in all but two specimens examined, both of which are from pegmatites. Trace level concentrations of elements not previously reported in natural titanites including Ru, Pd, Ag, and Te were detected by this technique. The lattice parameters of titanites vary directly with the effective octahedral cation radius. As in zircon, partial metamictization of some titanites causes increases in unit cell dimensions and decreases in density. Under electron bombardment, the characteristic x-ray yields are lower for metamict titanites than for their structurally restored 0 equivalents which were heated at 1100 C for three hours. The formation of out-of-step linear domains parallel to 100 (the octahedral chain direction) is favored by substitutions of Al + Fe for Ti. Pure CaT10SiO<sub>4</sub> is primitive (P2<sub>1</sub>/a) with weak, but sharp k + ℓ odd reflections. Increasing Al + Fe substitution increases the frequency of domains and the k + ℓ odd reflections become diffuse, eventually disappearing as the average structure attains space group A2/a.

Degree

thesis:*
Name thesis:degree_name
M.S.
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geological Sciences
Department dc:contributor.department
Geological Sciences
Grantor dc:publisher
Virginia Polytechnic Institute and State University
Year dc:date.issued
1975

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Higgins, John Britt

Rights

dc:rights
Statement dc:rights
  • In Copyright
Language dc:language.iso
en

Identifiers

dc:identifier.*
Handle dc:identifier.uri
https://hdl.handle.net/10919/118328
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/118328

Chain of custody

source
Harvested from
Virginia Tech
Base URL
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Last updated
2026-07-24
Source record
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related terms
citation

Higgins, John Britt. The crystal chemistry of titanite. masters thesis, Virginia Polytechnic Institute and State University, 1975. https://hdl.handle.net/10919/118328