Provenance of ArenitesG.G. Zuffa Proceedings of the NATO Advanced Study Institute on Reading Provenance from Arenites, Cetraro, Cosenza, Italy, June 3-11, 1984 |
From inside the book
Results 1-5 of 26
Page 23
... ( turbidity currents ) . Turbulence acts as a supporting force that stimulates individual behaviour of grains . This results in differential settling , with coarser and heavier particles moving closer to the bottom . In concentrated ...
... ( turbidity currents ) . Turbulence acts as a supporting force that stimulates individual behaviour of grains . This results in differential settling , with coarser and heavier particles moving closer to the bottom . In concentrated ...
Page 28
... turbidity current . This rigid interpretation , however , is not correct . Grading is the mark of turbulence and , consequently , of suspension flows ; but not all suspension flows are turbidity currents , i.e. gravity flows active in ...
... turbidity current . This rigid interpretation , however , is not correct . Grading is the mark of turbulence and , consequently , of suspension flows ; but not all suspension flows are turbidity currents , i.e. gravity flows active in ...
Page 30
... turbidity currents in deep - sea domains ( it is more textural than compositional , anyway ) . On the other hand , climatic - meteoro = logical reasons make also subaerial and shallow environments prone to catastrophic phenomena : see ...
... turbidity currents in deep - sea domains ( it is more textural than compositional , anyway ) . On the other hand , climatic - meteoro = logical reasons make also subaerial and shallow environments prone to catastrophic phenomena : see ...
Page 39
You have reached your viewing limit for this book.
You have reached your viewing limit for this book.
Page 42
You have reached your viewing limit for this book.
You have reached your viewing limit for this book.
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 |
Other editions - View all
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