Provenance of ArenitesProceedings of the NATO Advanced Study Institute on Reading Provenance from Arenites, Cetraro, Cosenza, Italy, June 3-11, 1984 |
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Page 1
INFLUENCE OF CLIMATE AND RELIE F O N C 0 MP 0S IT I 0 NS OF SAND'S
RELEASE D A T S 0 URCE AREAS ... the pro c e s ses, such as climatic and
biochemic a l, that contribute to any modification of the parent material at the
beginning ...
INFLUENCE OF CLIMATE AND RELIE F O N C 0 MP 0S IT I 0 NS OF SAND'S
RELEASE D A T S 0 URCE AREAS ... the pro c e s ses, such as climatic and
biochemic a l, that contribute to any modification of the parent material at the
beginning ...
Page 3
The rate of erosion of the highl and is controlled by relief and climate in the are a ;
up lift and erosion gradually unro of the rocks and eventually expose those in the
core of the highland. Thus exposure and the duration of exposure of a rock ...
The rate of erosion of the highl and is controlled by relief and climate in the are a ;
up lift and erosion gradually unro of the rocks and eventually expose those in the
core of the highland. Thus exposure and the duration of exposure of a rock ...
Page 4
Many except ions to the now well established relationship between tectonic sett
in gs and sands to n e composition (e.g. Dick in son et al., 1983) may be traced to
the V agaries of climate in the source areas (Mack, 1984). Genesis of sediments ...
Many except ions to the now well established relationship between tectonic sett
in gs and sands to n e composition (e.g. Dick in son et al., 1983) may be traced to
the V agaries of climate in the source areas (Mack, 1984). Genesis of sediments ...
Page 7
Comparable data are not yet a V ail able for other Climatic ZO n e S. It is quite
likely that the pro portion of clay relative to the sand fraction in the rego lith or soil
developed in hot humid climate would be much higher. However, there is no ...
Comparable data are not yet a V ail able for other Climatic ZO n e S. It is quite
likely that the pro portion of clay relative to the sand fraction in the rego lith or soil
developed in hot humid climate would be much higher. However, there is no ...
Page 8
Plutonic SOurce Arid Climate F R Fig. 2. A Ver age compositions of medium s
and – sized (0.25-0.50 mm) fraction of first cycle stream s and derived from pluto
nic ign e o us and metam or phic sources but produced under differ ent climatic ...
Plutonic SOurce Arid Climate F R Fig. 2. A Ver age compositions of medium s
and – sized (0.25-0.50 mm) fraction of first cycle stream s and derived from pluto
nic ign e o us and metam or phic sources but produced under differ ent climatic ...
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Contents
| 19 | |
LOCAL MORPHOLOGIC CONTROLS AND EFFECTS OF BASIN GEOMETRY | 47 |
TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL | 64 |
QUENCES | 86 |
TYPES OF POROSITY IN SANDSTONES AND THEIR SIGNIFICANCE | 114 |
PROVENANCE OF FELDSPATHIC SANDSTONES THE EFFEC OF DIAGEN | 139 |
SPECIAL TOPICS | 191 |
ENVIRONMENTAL INTERPRETATION OF QUARTZ GRAIN SURFACE TEXTURES | 212 |
READING PROVENANCE FROM DETRITAL QUARTZ | 233 |
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 36 3 | 363 |
INDEX OF NAMES | 393 |
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Common terms and phrases
albitization arenites arkosic authigenic Basu calcite carbonate cathodoluminescence channel chemical chert clastic clasts clay climate composition continental Cratonic Cretaceous crystal d e tr deep-sea depositional depth derived detrital detrital modes diagenesis diagenetic Dickinson dissolution electron environments Eocene epidote extrabasinal facies feldspar Figure flows flysch Formation G. G. Zuffa garnet Geol Geology glaucony green grains heavy minerals hydraulic indicate interpretation intrabasinal Jour K-feldspar Krinsley line quartz logy magmatic arcs metamorphic rocks Monterey Fan Mutti Normark Odin origin orogenic particles Petro petrofacies petrographic Petrology plagioclase Plate plutonic pores porosity processes provenance quartz quartz grains quartzose ratios recycled orogenic result Ricci Lucchi rock fragments samples sand grains sandstones sea level secondary porosity sediment Sedimentology sequences slope source area source rocks stage submarine fans substrate Suczek Suttner tectonic terrigenous tion transport turbidite turbidite systems turbidity currents types undulo sity uplift volcanic weathering Zinkernagel zone Zuffa
Bibliographic information
| Title | Provenance of Arenites Volume 148 of Nato Science Series C: |
| Editor | G.G. Zuffa |
| Edition | illustrated |
| Publisher | Springer Science & Business Media, 2013 |
| ISBN | 9401728097, 9789401728096 |
| Length | 408 pages |
| Subjects | › › › Science / Earth Sciences / General Science / Earth Sciences / Sedimentology & Stratigraphy Technology & Engineering / Agriculture / Agronomy / Soil Science |
| Export Citation | BiBTeX EndNote RefMan |