26 Undergraduate Research Session I (Posters)
Sunday, 19 March 2017
1:30 PM - 5:30 PM
Urban, 17th Floor
CHEMICAL AND THIN SECTION ANALYSIS OF THE COAL CREEK SERPENTINITE
Paper number: 26-17
Program: Theme Sessions
Time: 1:30 PM – 5:30 PM
Authors
Abstract
Through XRF spectroscopy, the results show high percentages of MgO and SiO2 and low amounts of CaO and Al2O3. The samples range from roughly 3%-8% in Fe2O3 and the oxidized material can be seen in some of the thin section samples. The chemical compositions suggests that the parent rock is serpentinized harzburgite that consists of predominantly antigorite, lizardite, and cross-cutting chrysotile as verified through thin section analysis. The cross-cutting nature of the chrysotile suggests that the antigorite formed at intermediate temperatures (400-550℃) that formed at depths of >50km (Jung et al.).
Geological Society of America Abstracts with Programs. Vol. 49, No. 2
doi: 10.1130/abs/2017NE-291584
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