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 5
Page 1
... line quartz , is difficult because lattice dislocation increases solubility MAIN FACTORS CONTROLLING THE COMPOSITION OF ARENITES INFLUENCE OF CLIMATE AND RELIEF ON COMPOSITIONS OF SANDS LEASED AT SOURCE AREAS A Basu.
... line quartz , is difficult because lattice dislocation increases solubility MAIN FACTORS CONTROLLING THE COMPOSITION OF ARENITES INFLUENCE OF CLIMATE AND RELIEF ON COMPOSITIONS OF SANDS LEASED AT SOURCE AREAS A Basu.
Page 2
G.G. Zuffa. line quartz , is difficult because lattice dislocation increases solubility as well as brittle strength . Given the extreme paucity of data from controlled studies on the effects of climate and relief and the seemingly ...
G.G. Zuffa. line quartz , is difficult because lattice dislocation increases solubility as well as brittle strength . Given the extreme paucity of data from controlled studies on the effects of climate and relief and the seemingly ...
Page 13
... quartz grains and polycrystal- line quartz grains with sutured sutured contacts between subgrains . Under normal atmospheric conditions and in common soils , quartz does not react with water to form new minerals but does go into ...
... quartz grains and polycrystal- line quartz grains with sutured sutured contacts between subgrains . Under normal atmospheric conditions and in common soils , quartz does not react with water to form new minerals but does go into ...
Page 206
You have reached your viewing limit for this book.
You have reached your viewing limit for this book.
Page 234
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