Coupled trace element mobilisation and strain softening in quartz during retrograde fluid infiltration in dry granulite protoliths

Author:

Sørensen Bjørn Eske,Larsen Rune B.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference39 articles.

1. Applin KR, Hicks BD (1987) Fibers of dumortierite in quartz. Am Mineral 71:786–794

2. Armington AF, Balascio JF (1984) The growth of high purity, low dislocation quartz. In: Proceedings of the 38th annual frequency control symposium, vol., USA, pp 3–7

3. den Brok B, Spiers CJ (1991) Experimental evidence for water weakening of quartzite by microcracking plus solution-precipitation creep. J Geol Soc London 148:541–548. doi: 10.1144/gsjgs.148.3.0541

4. Flem B, Larsen RB, Grimstvedt A, Mansfeld J (2002) In situ analysis of trace elements in quartz by using laser ablation inductively coupled plasma mass spectrometry. Chem Geol 182(2–4):237–247. doi: 10.1016/S0009-2541(01)00292-3

5. Goetze J, Plotze M, Habermann D (2001) Origin, spectral characteristics and practical applications of the cathodolumimescence (CL) of quartz—a review. Mineral Petrol 71(3–4):225–250. doi: 10.1007/s007100170040

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