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 v
... TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL SE- QUENCES E. Mutti 65 DIAGENETIC PROCESSES THAT AFFECT PROVENANCE DETERMINATIONS IN SANDSTONE E. F. McBride 95 TYPES OF POROSITY IN SANDSTONES AND THEIR SIGNIFICANCE IN ...
... TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL SE- QUENCES E. Mutti 65 DIAGENETIC PROCESSES THAT AFFECT PROVENANCE DETERMINATIONS IN SANDSTONE E. F. McBride 95 TYPES OF POROSITY IN SANDSTONES AND THEIR SIGNIFICANCE IN ...
Page 19
... turbidite sand , the time elapsed between particle production for example , G. G. Zuffa ( ed . ) , Provenance of Arenites , 19–45 . © 1985 by D. Reidel Publishing Company . 19 and final emplacement can be short or long , the INFLUENCE ...
... turbidite sand , the time elapsed between particle production for example , G. G. Zuffa ( ed . ) , Provenance of Arenites , 19–45 . © 1985 by D. Reidel Publishing Company . 19 and final emplacement can be short or long , the INFLUENCE ...
Page 26
... turbidite sands . Secondly , the traction base TB is an average limit ; in shelves dominated by wave energy , it is comprised between fair - weather and maximum storm wave bases , and more or less corresponds to the limit of average ...
... turbidite sands . Secondly , the traction base TB is an average limit ; in shelves dominated by wave energy , it is comprised between fair - weather and maximum storm wave bases , and more or less corresponds to the limit of average ...
Page 27
... turbidite flows , etc. ) do not go much beyond the base of the feeding slope because of the strong intergranular friction , and even to get there they need help by interstitial overpressure or liquefaction . Without overpressure , only ...
... turbidite flows , etc. ) do not go much beyond the base of the feeding slope because of the strong intergranular friction , and even to get there they need help by interstitial overpressure or liquefaction . Without overpressure , only ...
Page 28
... turbidite , therefore , is not simply a graded sand but a graded sequence going from basal sand to topmost mud ( Bouma seq = uence ) . A graded sand , or a graded layer , has long be regarded as the " trade mark " of the turbidity ...
... turbidite , therefore , is not simply a graded sand but a graded sequence going from basal sand to topmost mud ( Bouma seq = uence ) . A graded sand , or a graded layer , has long be regarded as the " trade mark " of the turbidity ...
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