Marginal basin geology: volcanic and associated sedimentary - download pdf or read online

By B. Peter Kokelaar

ISBN-10: 0632010738

ISBN-13: 9780632010738

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Extra resources for Marginal basin geology: volcanic and associated sedimentary and tectonic processes in modern and ancient marginal basins

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Res. 79, 3087-97. SHERIDAN, M. F. 1979. Emplacement of pyroclastic flows: a review. Spec. Pap. geol. Soc. Am. 180, 125-36. , SPARKS, R. S. , CAREY, S. N. t~ HUANG, T. C. 1980. Volcanogenic sedimentation in the Lesser Antilles Arc. J. Geol. 8 8 , 523-40. SMITJJ, R. L. 1960. Ash flows. Bull. geol. Soc. Am. 71, 795-842. SPARKS, R. S. J. 1976. Grain size variations in ignimbrites and implications for the transport of pyroclastic flows. Sedimentology, 23, 147-88. - - . , SIGURDSSON, H. & EARLY, S. 1980a.

K. 1981. Nonmarine sedimentation in an active forre arc basin. Spec. Publ. Soc. econ. Paleontol. , Tulsa, 31, 31-45. WALKER,G. P. L. 1979. A volcanic ash generated by explosions where ignimbrite entered the sea. Nature, Lond. 281, 642-6. WATKINS, N. D. t~ HUANG, T. C. 1977. Tephras in abyssal sediments east of the North Island, New Zealand: Chronology, paleowind velocity, and paleoexplosivity. Z. Jl Geol. Geophys. 20, 179-98. , SPARKS, R. S. , HUANG, T. , CAREY,S. & NINKOVICH,D. 1978. Volume and extent of the Minoan tephra from Santorini Volcano: new evidence from deep-sea sediment cores.

Their flow mechanism is similar to that of their subaerial counterparts, except that they incorporate steam and not air. Near the source area, their deposits are non-sorted and resemble subaerial flow deposits. In some cases evidence of high temperature is recognized. Within a short distance (less than a few km) they are sorted and five subdivisions can be determined. In upward succession these are: (i) massive graded pumice tuff; (ii) parallel-laminated pumice tuff; (iii) parallel-laminated sandy tuff; (iv) parallel-laminated fine tuff; and (v) massive very fine tuff.

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Marginal basin geology: volcanic and associated sedimentary and tectonic processes in modern and ancient marginal basins by B. Peter Kokelaar

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