By K. R. Walker, J. F. Read, L. A. Hardie, K. Roberson, D. M. Steinhauff(auth.)
About The Product
Published via the yank Geophysical Union as a part of the Field journey Guidebooks Series.
This e-book was once designed to steer the members in a nine day box journey held together with the 1989 overseas Geological Congress. The journey is ready both divided between 3 parts: jap Tennessee, western Virginia, and Maryland. the 3 components of the consultant (a half for every of the components) were ready by means of okay. R. Walker, J. Fred learn, and Lawrence A. Hardie. Many cease descriptions can be utilized independently. The textual content for a few stops is a separate, self-contained article that stands on my own. different components of the advisor are extra non-stop, and no more without delay keyed to box stops.
Read or Download Cambro-Ordovician Carbonate Banks and Siliciclastic Basins of the United States Appalachians: Knoxville, Tennessee to Hagerstown, Maryland, June 30-July 9, 1989 PDF
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Extra info for Cambro-Ordovician Carbonate Banks and Siliciclastic Basins of the United States Appalachians: Knoxville, Tennessee to Hagerstown, Maryland, June 30-July 9, 1989
SMOOTH PORTION OF SUPRAFAN LOBES Cl. T. L. a: ~ ffl LOWER FAN FINING- OR COARSENINGUPWARD Figure 23 Model for submarine fan deposition (slightly modified by Boling and Keller, 1980, from Walker, 1978). From Bowlin and Keller, 1978. Left: map view of facies; Right: ideal vertical sequence through a prograding fan. for preservation of these features. At the north end of this cut several thick massive sandstones form an amalgamated package that overlies a thick sequence of intercalated shale and individual massive sandstone beds.
Glauconite and reworking of the bottom could have been inhibited by hardgrounds are common in the grainy carbonates. J a: < w I I I l I I l 1J_T. II MONKTON SEQUENCE 2 DUNHAM () ANTIETAM CHILHOWEE 570 CHESHIRE SEQUENCE HARPERS 1 WEVERTON Fig. IB Time-stratigraphic chart of Cambrian and Early Ordovician passive margin sequence, showing major sequences and fonnations. MID. TO LATE - - - - - - - - - - - - - - - -..... MARTINSBURG ORO. ------...... lLI o Z lLI o=> lLI (f) NEALMONTI EGGLESTON COLLIERSTOWNI MOCCASIN ORANDA WITTEN (f) MIDDLE ORO.
S. 421S. S. 421S. Turn left, continue on 421S. " After turn, view Holston Mountain on horizon. Outcrop of Cambrian lower Knox Group dolostones. Badly cleaved Sevier Formation shales on left. Turn right at sign onto North Access Road to South Holston Dam. 9 Outcrops of Knox Group dolostones on left. 7 Take left fork to North Access Road. (Right fork is South Access Road). 4 Outcrops of Blockhouse and Tellico formations nearly continuous from this point to the Dam. STOP 8. Shanmugam and Walker (1978) referred to these types of laminae as ultradistal turbidites.