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 21
... depth at which sand can be transported by " normal " proc = esses ) , closely associated with 1 , and 3. the gravity base level GB where deposition by gravity processes starts ( slumps , slides , tur = bidity currents and other sediment ...
... depth at which sand can be transported by " normal " proc = esses ) , closely associated with 1 , and 3. the gravity base level GB where deposition by gravity processes starts ( slumps , slides , tur = bidity currents and other sediment ...
Page 26
... depths , as far as the shelf edge , by exceptional storm events , but in this case it is mobilized en masse . Littoral and shelf sands are separated by a mud belt from deep- water sands ; moreover , the deep mode is not supplied by the ...
... depths , as far as the shelf edge , by exceptional storm events , but in this case it is mobilized en masse . Littoral and shelf sands are separated by a mud belt from deep- water sands ; moreover , the deep mode is not supplied by the ...
Page 31
... depth . They are members of a broader family of indicators , both mechani = cal , chemical and biological such as plant roots , specific trace fossils , pedogenic cements , nodules and crusts , oxidation , mud cracks , and so on . If ...
... depth . They are members of a broader family of indicators , both mechani = cal , chemical and biological such as plant roots , specific trace fossils , pedogenic cements , nodules and crusts , oxidation , mud cracks , and so on . If ...
Page 41
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Page 49
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Contents
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 |
SUBJECT INDEX | 363 |
INDEX OF NAMES | 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