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University at Albany, State University of New York Scholars Archive

Geology Theses and Dissertations Atmospheric and Environmental Sciences

1982

The of the Oceanographer Transform

Richard H. Moody Jr. University at Albany, State University of New York

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Recommended Citation Moody, Richard H. Jr., "The geology of the Oceanographer Transform Fault" (1982). Geology Theses and Dissertations. 61. https://scholarsarchive.library.albany.edu/cas_daes_geology_etd/61

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Figure 2-16

ANGUS 124, 35º08'N, 35º33'W. Field of view 5 x 7 meters. Probable in carbonate mud with debris flow at base. Debris flow shows extensive signs of reworking by bottom grazers. 115

Figure 2-17

ANGUS 122, 35º08'N, 35º07'W. Field of view 4 x 6 meters. Fault scarp in poorly consolidated carbonate showing extensive evidence of gullying and degradation. Lighter streaks are exhumed (?) sediment flowing downhill. 116

Figure 2-18

ANGUS 126, 35º02.6'N, 35º22.5'W. Field of view 5 x 7 meters. Lithified carbonate encrusted with manganese that is interpreted to show substantial erosion of original sediment probably by winnowing. 117

Figure 2-19

ANGUS 126, 35º02.2'N, 35º22.5'W. Field of view (4-6) x (4-10) meters. Steep wall of lithified breccia. Minor amounts of sessile faunas.

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Figure 2-21

ANGUS 124, 35º12'N, 35º33.6'W. Field of view 5 x 7 meters. Low amplitude possible wave ripples in carbonate mud. 121

Figure 2-22

ANGUS 126, 35º10'N, 35º20'W. Field of view 5 x 7 meters. Longditudinal triangular ripples in unconsolidated pteropod shells. These form parallel to the direction of the current flow. 122

Figure 2-23

ANGUS 126, 35º04.6'N, 35º26.2'W. Field of view 5 x (5-8) meters. Parallel grooves (abyssal furrows) in carbonate ooze. These are believed to form parallel to the direction of the prevailing current. 123

Figure 2-24

ANGUS 126, 35º02.2'N, 35º22.5'W. Field of view 4 x (3-8) meters. Steep breccia wall with luxuriant growth of sessile faunas. 124

Figure 2-25

ANGUS 122, 35º08'N, 35º31.7'W. Field of view 5 x 7 meters. Shoestring rills forming in unconsolidated sediments at the head of a scarp.

126