Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model
Abstract
Abstract Field observations are combined with microscopic analyses to investigate the mechanism of formation of wiggly compaction bands (CBs) in the porous Jurassic aeolian Aztec Sandstone exposed at Valley of Fire State Park, Nevada. Among the three types of CBs (T1, T2, and T3), we focused on the wiggly CBs (T3), which show a chevron (T3 1 ) or wavy (T3 2 ) pattern with typical corner angles of approximately 90° or 130°, respectively. Where corner angles of wiggly CBs increase to 180°, they become straight CBs (T3 3 ). Image analyses of thin sections using an optical microscope show host rock porosity increases downslope in this dune, and the predominant type of wiggly CBs also varies from chevron to straight CBs. Specifically, band type varies continuously from chevron to wavy to straight where the porosity and grain sorting of the host rock increase systematically. Based on the crack and anticrack models, we infer that the change from chevron to straight CBs is due to increasing failure angle of the sandstone and this may correlate with increasing grain sorting. Wavy CBs with intermediate failure angle and host rock porosity are an intermediate stage between chevron and straight CBs. Previous sedimentologicalmore »
- Authors:
-
- Nanjing Univ., Nanjing (China); Stanford Univ., Stanford, CA (United States)
- Stanford Univ., Stanford, CA (United States)
- Stanford Univ., Stanford, CA (United States); Sinopec Group, Beijing (China)
- Publication Date:
- Research Org.:
- The Leland Stanford Junior Univ., Palo, Alto, CA (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1468439
- Alternate Identifier(s):
- OSTI ID: 1402308
- Grant/Contract Number:
- FG02-04ER15588; DE‐FG02‐04ER15588
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 120; Journal Issue: 12; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; wiggly compaction band; formation mechanism; sandstone deformation; porosity; grain sorting
Citation Formats
Liu, Chun, Pollard, David D., Deng, Shang, and Aydin, Atilla. Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model. United States: N. p., 2015.
Web. doi:10.1002/2015JB012372.
Liu, Chun, Pollard, David D., Deng, Shang, & Aydin, Atilla. Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model. United States. https://doi.org/10.1002/2015JB012372
Liu, Chun, Pollard, David D., Deng, Shang, and Aydin, Atilla. Tue .
"Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model". United States. https://doi.org/10.1002/2015JB012372. https://www.osti.gov/servlets/purl/1468439.
@article{osti_1468439,
title = {Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model},
author = {Liu, Chun and Pollard, David D. and Deng, Shang and Aydin, Atilla},
abstractNote = {Abstract Field observations are combined with microscopic analyses to investigate the mechanism of formation of wiggly compaction bands (CBs) in the porous Jurassic aeolian Aztec Sandstone exposed at Valley of Fire State Park, Nevada. Among the three types of CBs (T1, T2, and T3), we focused on the wiggly CBs (T3), which show a chevron (T3 1 ) or wavy (T3 2 ) pattern with typical corner angles of approximately 90° or 130°, respectively. Where corner angles of wiggly CBs increase to 180°, they become straight CBs (T3 3 ). Image analyses of thin sections using an optical microscope show host rock porosity increases downslope in this dune, and the predominant type of wiggly CBs also varies from chevron to straight CBs. Specifically, band type varies continuously from chevron to wavy to straight where the porosity and grain sorting of the host rock increase systematically. Based on the crack and anticrack models, we infer that the change from chevron to straight CBs is due to increasing failure angle of the sandstone and this may correlate with increasing grain sorting. Wavy CBs with intermediate failure angle and host rock porosity are an intermediate stage between chevron and straight CBs. Previous sedimentological studies also have suggested that grain size and sorting degree increase downslope on the downwind side of sand dunes due to a sieving process of the wind‐blown grains. Therefore, the transition of wiggly CB types in this regard correlates with increasing sorting and perhaps with increasing porosity downslope.},
doi = {10.1002/2015JB012372},
journal = {Journal of Geophysical Research. Solid Earth},
number = 12,
volume = 120,
place = {United States},
year = {Tue Nov 17 00:00:00 EST 2015},
month = {Tue Nov 17 00:00:00 EST 2015}
}
Web of Science
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Works referencing / citing this record:
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