Provenance of ArenitesGian Gaspare Zuffa Dipartimento di Scienze della Terra Universitä della Calabria 87030 Castiglione Cosentino Stazione, Cosenza, ITALY The tradition has been to consider Sedimentology and Sedimen tary Petrology as quite separate areas of research. It is however impossible to arrive at an optimal description of sedimentary rocks without integrating the two fields since sedimentary processes and compositional aspects are strongly intertwined. The study of arenites is of particular importance in obtaining paleogeographic and paleotectonic reconstructions aimed at deter mining the geodynamics of the earth's crust. It also has important implications in exploration for and exploitation of hydrocarbons. At the NATO ASI Meeting on Reading Provenance from Arenites held in Calabria (Italy), June 3-ll, 1984, field sedimentologists and sedimentary petrologists were given opportunity to pool their resources in order to obtain better analyses of both source areas and depositional basins. The papers collected in this volume represent an edited ver sion of the lectures given and provide a comprehensive picture of the present state of the art since they include such important top ics as: l) the climate and relief of the source areas, 2) mechani cal transport of sediments and depositional processes, 3) postdep ositional processes, and 4) the methodology adopted for petrogra phic optical analyses. Particular attention has been paid to the limitations and errors introduced into paleogeographic and paleo tectonic reconstructions by incomplete and incorrect data. |
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Page 96
Common reactions of detrital grain types during diagenesis are listed in Table 1 .
DISSOLUTION Nearly all detrital grain types can undergo some degree of
dissolution by meteoric water in outcrop and at shallow to intermediate depths in
the ...
Common reactions of detrital grain types during diagenesis are listed in Table 1 .
DISSOLUTION Nearly all detrital grain types can undergo some degree of
dissolution by meteoric water in outcrop and at shallow to intermediate depths in
the ...
Page 97
Common Diagenetic Processes That Affect Detrital Grain Types . Processes are
listed in sequence of most common ( first ) to less common . K - feldspar :
calcitized zeolitized dissolved kaolinized albitized Plagioclase : calcitized
dissolved ...
Common Diagenetic Processes That Affect Detrital Grain Types . Processes are
listed in sequence of most common ( first ) to less common . K - feldspar :
calcitized zeolitized dissolved kaolinized albitized Plagioclase : calcitized
dissolved ...
Page 117
Table 1. Classification of porosity in sandstones POSITIVE EFFECTS ON
RESERVOIR QUALITY PORE TYPES DISTRIBUTION Primary intergranular
Common and isolated Small to large Primary intragranular Very rare and isolated
Very small ...
Table 1. Classification of porosity in sandstones POSITIVE EFFECTS ON
RESERVOIR QUALITY PORE TYPES DISTRIBUTION Primary intergranular
Common and isolated Small to large Primary intragranular Very rare and isolated
Very small ...
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Contents
INFLUENCE OF TRANSPORT PROCESSES AND BASIN GEOMETRY ON SAND | 19 |
LOCAL MORPHOLOGIC CONTROLS AND EFFECTS OF BASIN GEOMETRY | 47 |
TURBIDITE SYSTEMS AND THEIR RELATIONS TO DEPOSITIONAL | 67 |
Copyright | |
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Common terms and phrases
abundance active albitization alteration analysis arenites associated basin Bull carbonate channel chemical clay climate common composition continental crystals depositional depth derived determined detrital developed diagenetic Dickinson dissolution effects electron environments et al example facies feldspar Figure flows Formation Geol Geology glaucony green heavy minerals important increase indicate interpretation Italy Jour K-feldspar less lithic lobes lower luminescence marine mechanical metamorphic method minerals modified observed occur origin orogenic particles patterns Petrology plagioclase Plate Pleistocene plutonic pores porosity possible present problem processes produced provenance quartz grains ratios relative replacement result rock fragments samples sand sandstones sea level secondary sedimentary sediments sequences setting slope stage structural substrate suites surface Table tectonic textures tion transport turbidite turbidity currents types upper volcanic volcaniclastic volume weathering zone Zuffa