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