TOURMALINE STUDIES: PAST, PRESENT AND THE NEXT 100 YEARS
In the early-mid 20th century with the development of instrumentation, tur studies greatly expanded as characterization of its chemical and physical properties improved. Tur’s piezoelectric properties were utilized for detection and measurement of conventional and atomic explosion pressures. In clastic sedimentary rocks tur was identified as an important heavy mineral that became a means to determine provenance and make stratigraphic correlations. By the 1960-70s, tur’s overall crystal structure and structural formulae were largely deciphered.
More recent studies have demonstrated its vast petrogenetic utility, far-ranging compositions, and extreme pressure-temperature-compositional (P-T-X) stability. Tur has become a valuable indicator mineral in rocks and sediments because of its capacity to obtain a chemical signature of the rock in which it formed and evolved, its ability to retain this chemical imprint through weathering and transport, and its capability to provide specific information on the time, temperature and fluid history at each stage of tur’s development. New analytical tools have opened exciting and significant chemical, crystallographic and spectroscopic possibilities such that the future of tur studies will certainly continue to influence scientific inquiry. Thus, as tur is stable and increasingly valuable for mineralogical studies, so is MSA.