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 vi
... . Valloni ... 309 INTERPRETING PROVENANCE RELATIONS FROM DETRITAL MODES OF SANDSTONES W. R. Dickinson SUBJECT INDEX INDEX OF NAMES 333 363 393 PREFACE Gian Gaspare Zuffa Dipartimento di Scienze della Terra Università vi CONTENTS.
... . Valloni ... 309 INTERPRETING PROVENANCE RELATIONS FROM DETRITAL MODES OF SANDSTONES W. R. Dickinson SUBJECT INDEX INDEX OF NAMES 333 363 393 PREFACE Gian Gaspare Zuffa Dipartimento di Scienze della Terra Università vi CONTENTS.
Page 3
... ( Dickinson , 1972 , 1980 ) . The rate of erosion of the highland is controlled by relief and climate in the area ; uplift and erosion gradually unroof the rocks and eventually expose those in the core of the highland . Thus exposure and ...
... ( Dickinson , 1972 , 1980 ) . The rate of erosion of the highland is controlled by relief and climate in the area ; uplift and erosion gradually unroof the rocks and eventually expose those in the core of the highland . Thus exposure and ...
Page 4
... Dickinson et al . , 1983 ) may be traced to the vagaries of climate in the source areas ( Mack , 1984 ) . Genesis of sediments begins with regolith and / or soil formation on a bedrock . The composition of the bedrock is controlled ...
... Dickinson et al . , 1983 ) may be traced to the vagaries of climate in the source areas ( Mack , 1984 ) . Genesis of sediments begins with regolith and / or soil formation on a bedrock . The composition of the bedrock is controlled ...
Page 7
... Dickinson method ( Ingersoll et al . , 1984 ; Zuffa , this volume ) . The population of rock fragments in the Indiana data effectively separates plutonic and metamorphic source rocks ( fig . 2 ) . If counted otherwise , we suspect , not ...
... Dickinson method ( Ingersoll et al . , 1984 ; Zuffa , this volume ) . The population of rock fragments in the Indiana data effectively separates plutonic and metamorphic source rocks ( fig . 2 ) . If counted otherwise , we suspect , not ...
Page 8
... cycle sediments . If counted according to the Gazzi - Dickinson method ( Ingersoll et al . , 1984 ) most of the distinctions seen on this plot would have been lost . climatic distinction might be obliterated to a large extent . 8 A. BASU.
... cycle sediments . If counted according to the Gazzi - Dickinson method ( Ingersoll et al . , 1984 ) most of the distinctions seen on this plot would have been lost . climatic distinction might be obliterated to a large extent . 8 A. BASU.
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