Provenance of ArenitesG.G. Zuffa Proceedings of the NATO Advanced Study Institute on Reading Provenance from Arenites, Cetraro, Cosenza, Italy, June 3-11, 1984 |
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Page 7
... clay relative to the sand fraction in the regolith or soil developed in hot humid climate would be much higher . However , there is no evidence yet to show that the relationship between modal com- positions of sand sized fractions of ...
... clay relative to the sand fraction in the regolith or soil developed in hot humid climate would be much higher . However , there is no evidence yet to show that the relationship between modal com- positions of sand sized fractions of ...
Page 12
... clay fraction pertain to 0.075-0.21 mm size range . Hill crest Hill slope Floodplain Beach Quartz 19 1.5 5 3 Feldspar 2 14 37 31 Rock 2 46.5 38 32 Fragments Accessary 38 27.5 18 32 Minerals Clay 38 10.5 2 2 the hilltop material . Note ...
... clay fraction pertain to 0.075-0.21 mm size range . Hill crest Hill slope Floodplain Beach Quartz 19 1.5 5 3 Feldspar 2 14 37 31 Rock 2 46.5 38 32 Fragments Accessary 38 27.5 18 32 Minerals Clay 38 10.5 2 2 the hilltop material . Note ...
Page 95
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Page 98
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Page 101
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Contents
INFLUENCE OF TRANSPORT PROCESSES AND BASIN GEOMETRY ON SAND | 19 |
LOCAL MORPHOLOGIC CONTROLS AND EFFECTS OF BASIN GEOMETRY | 47 |
TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL | 67 |
QUENCES | 86 |
TYPES OF POROSITY IN SANDSTONES AND THEIR SIGNIFICANCE | 114 |
PROVENANCE OF FELDSPATHIC SANDSTONES THE EFFECT OF DIAGEN | 139 |
COMPOSITIONAL RESULTS | 164 |
SPECIAL TOPICS | 191 |
READING PROVENANCE FROM DETRITAL QUARTZ | 231 |
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 |
363 | |
393 | |
ENVIRONMENTAL INTERPRETATION OF QUARTZ GRAIN SURFACE TEXTURES | 212 |
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Common terms and phrases
albitization America Bull arenites arkosic authigenic Basu calcite carbonate cathodoluminescence channel channel-fill chemical chert clastic clasts clay climate Cratonic Cretaceous crystals deep-sea depositional depth detrital detrital modes detrital quartz diagenesis diagenetic Dickinson dissolution electron environments Eocene epidote extrabasinal facies feldspar Figure flows fluvial flysch Formation garnet Geol Geology glaucony green grains heavy minerals hydraulic indicate interpretation intrabasinal Jour K-feldspar Krinsley magmatic arcs marine berthierine metamorphic rocks monocrystalline quartz Monterey Fan Mutti Normark Odin origin orogenic parent rocks particles petrofacies petrographic Petrology plagioclase Plate plutonic polycrystalline pores porosity processes provenance quartz quartz grains quartzose ratios recycled orogenic result Ricci Lucchi rock fragments samples sand grains sands derived sandstones sea level secondary porosity sedimentary Sedimentology sediments sequences slope source area source rocks stage submarine fans substrate Suczek Suttner terrigenous tion transport turbidite turbidite systems turbidity currents types undulosity uplift Valloni volcanic weathering Zinkernagel zone Zuffa