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 53
The deeply incised Monterey valley confines more of the turbidity currents
entering the two canyon systems than did the pre - erosion valleys . Flow
stripping ( the loss of the upper part of turbidity currents at channel bends ; see
next section ...
The deeply incised Monterey valley confines more of the turbidity currents
entering the two canyon systems than did the pre - erosion valleys . Flow
stripping ( the loss of the upper part of turbidity currents at channel bends ; see
next section ...
Page 58
Flow stripping apparently was less effective in diverting these sandier turbidity
currents from the channel system ( Piper and Normark , 1983 ) . This implies that
sandy turbidity currents are more concentrated ( Bowen et al . , 1984 ) .
Flow stripping apparently was less effective in diverting these sandier turbidity
currents from the channel system ( Piper and Normark , 1983 ) . This implies that
sandy turbidity currents are more concentrated ( Bowen et al . , 1984 ) .
Page 73
RELATIONS BETWEEN DEGREE OF SLOPE INSTABILITY AND VOLUME OF
TURBIDITY CURRENTS STAGE TYPE I ... volume mud - loden turbidity currents
SHALLOW SLUMP sea level STAGE I TYPE II SYSTEM OR STAGE II DEPOSITS
6 ...
RELATIONS BETWEEN DEGREE OF SLOPE INSTABILITY AND VOLUME OF
TURBIDITY CURRENTS STAGE TYPE I ... volume mud - loden turbidity currents
SHALLOW SLUMP sea level STAGE I TYPE II SYSTEM OR STAGE II DEPOSITS
6 ...
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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