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structural geology, propagation mechanics and - Stanford School of ...

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Although systematic arrays <strong>of</strong> DBs pervade the middle <strong>and</strong> upper Aztec, DB-poor<br />

exposures tens to hundreds <strong>of</strong> meters or more on a side are also common. The reasons for<br />

this patchwork quality to the DB fabric at a variety <strong>of</strong> scales is as yet poorly understood,<br />

but may be related to the æolian sedimentary architecture <strong>of</strong> the Aztec <strong>and</strong> differences in<br />

how distinct dune packages responded to tectonic loading during DB formation.<br />

Nonetheless, any given characteristic DB pattern recognized in outcrop can be seen to<br />

persist at length scales ranging from meters (the thickness <strong>of</strong> small cross-bed packages)<br />

to tens <strong>of</strong> meters (the thickness <strong>of</strong> large cross-bed packages) to hundreds <strong>of</strong> meters (for<br />

DBs that pass through multiple dune boundaries).<br />

4.1. Parallel<br />

Patterns <strong>of</strong> approximately parallel DBs crop out extensively throughout the Aztec<br />

over areas ranging from tens to hundreds <strong>of</strong> meters on a side. Individual b<strong>and</strong>s within the<br />

parallel sets commonly range up to ~1.5 cm thick <strong>and</strong> are spaced anywhere from<br />

centimeters to meters apart (Figure 6.3). It is not uncommon, however, to see groups <strong>of</strong><br />

individually distinct DBs running parallel to each other only millimeters apart, sometimes<br />

merging into what appears in outcrop to be a single b<strong>and</strong> 10 cm or more thick. Also,<br />

groups <strong>of</strong> closely spaced DBs <strong>of</strong>ten form distinct sets spaced a meter or more from the<br />

next adjacent, closely spaced set. DBs cropping out in parallel patterns throughout the<br />

Aztec cluster around three mean strike/dip orientations—350°/70°, 210°/60° <strong>and</strong><br />

240°/30° (using the convention <strong>of</strong> dip direction oriented 90° clockwise from the strike<br />

azimuth). The first two <strong>of</strong> these sets cut across depositional bedding at a high angle,<br />

while the third generally runs sub-parallel to bedding. The north-trending, steeply east-<br />

dipping DB orientation (350°/70°) strongly dominates in terms <strong>of</strong> abundance, persistence<br />

<strong>and</strong> distribution, <strong>and</strong> is the one shown in both Figures 6.2 <strong>and</strong> 6.3.<br />

4.2. Cross-hatch<br />

Cross-hatch patterns <strong>of</strong> DBs, which generally crop out over areas from meters to 10s<br />

<strong>of</strong> meters on a side, consist <strong>of</strong> two distinct sets <strong>of</strong> parallel b<strong>and</strong>s that commonly intersect<br />

each other at a high angle (Figure 6.4). In the Aztec, individual b<strong>and</strong>s within the cross-<br />

hatch patterns exhibit the same range <strong>of</strong> widths as b<strong>and</strong>s in the parallel patterns <strong>and</strong> the<br />

same tendency to occur as closely spaced pairs. Spacing between b<strong>and</strong>s ranges from 2 cm<br />

148

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