By A. C. Morton, Seldon P., Jr. Todd, P. D. W. Haughton
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Extra resources for Developments in sedimentary provenance studies
Contributions to Mineralogy and Petrology 53, 281-291. BASU, A. & MOLINAROLI, E. 1990. Provenance of detrital Fe-Ti oxides. This volume. BORG, G. 1986. Facetted garnets formed by etching. Examples from sandstones of Late Triassic age, South Germany. Sedimentology, 33, 141-146. BOSWELL, P. G. H. 1924. The petrography of the sands of the Upper Lias and Lower Inferior Oolite in the west of England. Geological Magazine, 31, 246-264. BUTLER, J. R. & THOMPSON, A. J. 1965. Zirconium: hafnium ratio in some igneous rocks.
B. & KORYLUK, V. N. 1973. Range of variation in the composition of staurolite from typical metapelites with pressure and temperature of metamorphism. Doklady, Academy of Sciences of the USSR, Earth Science Section, 212, 121-125. KNOX, R. W. , MORTON, A. C. & LOTT, G. K. 1982. Petrology of the Bridport Sands in the Winterborne Kingston Borehole, Dorset. Report of the Institute of Geological Sciences, 81/3, 107121. KRVNINE, P. D. 1946. The tourmaline group in sediments. Journal of Geology, 54, 65-87.
C. 1988. An application of heavy-mineral analysis to lithostratigraphy and reservoir modelling in the Oseberg Field, northern North Sea. ~larine and Petroleum Geology, 5, 157-169. KEPEZHINSKAS, K. B. & KORYLUK, V. N. 1973. Range of variation in the composition of staurolite from typical metapelites with pressure and temperature of metamorphism. Doklady, Academy of Sciences of the USSR, Earth Science Section, 212, 121-125. KNOX, R. W. , MORTON, A. C. & LOTT, G. K. 1982. Petrology of the Bridport Sands in the Winterborne Kingston Borehole, Dorset.