Provenance of ArenitesProceedings of the NATO Advanced Study Institute on Reading Provenance from Arenites, Cetraro, Cosenza, Italy, June 3-11, 1984 |
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Contents
19 | |
LOCAL MORPHOLOGIC CONTROLS AND EFFECTS OF BASIN GEOMETRY | 47 |
TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL | 64 |
QUENCES | 86 |
TYPES OF POROSITY IN SANDSTONES AND THEIR SIGNIFICANCE | 114 |
PROVENANCE OF FELDSPATHIC SANDSTONES THE EFFEC OF DIAGEN | 139 |
SPECIAL TOPICS | 191 |
ENVIRONMENTAL INTERPRETATION OF QUARTZ GRAIN SURFACE TEXTURES | 212 |
READING PROVENANCE FROM DETRITAL QUARTZ | 233 |
HEAVY MINERALS IN PROVENANCE STUDIES | 248 |
SIGNIFICANCE OF GREEN PARTICLES GLAUCONY BERTHIERINE CHLO | 279 |
GLOBAL SYNTHESIS ON MODERN AND ANCIENT MARINE SANDS | 308 |
INTERPRETING PROVENANCE RELATIONS FROM DETRITAL MODES | 333 |
SUBJECT INDEX 36 3 | 363 |
INDEX OF NAMES | 393 |
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Common terms and phrases
albitization arenites arkosic authigenic Basu calcite carbonate cathodoluminescence channel chemical chert clastic clasts clay climate composition continental Cratonic Cretaceous crystal d e tr deep-sea depositional depth derived detrital detrital modes diagenesis diagenetic Dickinson dissolution electron environments Eocene epidote extrabasinal facies feldspar Figure flows flysch Formation G. G. Zuffa garnet Geol Geology glaucony green grains heavy minerals hydraulic indicate interpretation intrabasinal Jour K-feldspar Krinsley line quartz logy magmatic arcs metamorphic rocks Monterey Fan Mutti Normark Odin origin orogenic particles Petro petrofacies petrographic Petrology plagioclase Plate plutonic pores porosity processes provenance quartz quartz grains quartzose ratios recycled orogenic result Ricci Lucchi rock fragments samples sand grains sandstones sea level secondary porosity sediment Sedimentology sequences slope source area source rocks stage submarine fans substrate Suczek Suttner tectonic terrigenous tion transport turbidite turbidite systems turbidity currents types undulo sity uplift volcanic weathering Zinkernagel zone Zuffa