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1

Chidsey, Thomas, and Paul Anderson. "Ancient delta deposits in the Ivie Creek area, Ferron Sandstone member of the Mancos Shale, western San Rafael Swell, east-central Utah." Geosites 1 (December 1, 2019): 1–18. http://dx.doi.org/10.31711/geosites.v1i1.74.

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In contrast to the beautiful array of colorful layers and spectacular cliffs of the Triassic and Jurassic (251 to 148 million years ago [Ma]) sections in the San Rafael Swell of east-central Utah, most of the Upper Cretaceous (96 to 86 Ma) Mancos Shale produces a drab, barren landscape. However, lying within the Mancos, the Ferron Sandstone, is the most studied unit in the San Rafael Swell. The Ferron has world-class outcrops of rock layers deposited near the shorelines of a sinking, fluvial- (stream) dominated delta system. Along the west flank of the San Rafael Swell, the 80-mile-long (130 k
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2

Phillips, Stephen P., John A. Howell, Adrian J. Hartley, and Magda Chmielewska. "Tidal estuarine deposits of the transgressive Naturita Formation (Dakota Sandstone): San Rafael Swell, Utah, U.S.A." Journal of Sedimentary Research 90, no. 8 (2020): 777–95. http://dx.doi.org/10.2110/jsr.2020.51.

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ABSTRACT Thin tidal estuarine deposits of the Naturita Formation (0–23 m) of the San Rafael Swell record the initial flooding of the Cretaceous Western Interior Seaway, Utah, and capture the transition from inland fluvial systems to fully marine conditions over a time period of 5 My or less. A tide-dominated estuarine environment is favored due to the combined presence of mud and/or carbonaceous drapes on ripples and dunes, bidirectional flow indicators, sigmoidal cross-stratification, herring-bone cross-stratification, and bimodal paleocurrent measurements. Facies associations are arranged in
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3

Doolittle, J. A., S. J. Neild, L. D. Sasser, and J. W. Tuttle. "Characterizing a Lithosequence within the San Rafael Swell of Utah with EMI." Soil Horizons 46, no. 4 (2005): 169. http://dx.doi.org/10.2136/sh2005.4.0169.

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4

Delaney, Paul T., and Anne E. Gartner. "Physical processes of shallow mafic dike emplacement near the San Rafael Swell, Utah." Geological Society of America Bulletin 109, no. 9 (1997): 1177–92. http://dx.doi.org/10.1130/0016-7606(1997)109<1177:pposmd>2.3.co;2.

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5

Chidsey, Thomas, and Paul Anderson. "Spectacular crinkled crust—A detachment fold train in the Carmel Formation, western San Rafael Swell, Utah." Geosites 1 (December 13, 2019): 1–9. http://dx.doi.org/10.31711/geosites.v1i1.75.

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Imagine slipping on a small rug overlying a hardwood floor. In the process of sliding along the floor the rug produces a series of small folds and the rug moves forward from its original position. The same could be said for the “crinkled crust,” or folded layers of rocks in a detachment fold train. A spectacular detachment fold train, consisting of over 100 small, regularly spaced convex-upward folds called anticlines in gypsum-rich rock layers of the Middle Jurassic (about 168 million years ago [Ma]) Carmel Formation, is exposed immediately north of Interstate 70 (I-70) in the San Rafael Swel
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6

Heil, Kenneth, Rich Fleming, J. Porter, and William Romme. "A Vegetation Study of Capitol Reef National Park." UW National Parks Service Research Station Annual Reports 10 (January 1, 1986): 37–40. http://dx.doi.org/10.13001/uwnpsrc.1986.2543.

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Capitol Reef National Park lies in a relatively unexplored region of southcentral Utah. The diversity in geology and the elevation gradient (3,500-9,000 feet) allows for diverse vegetation including endemic and rare taxa (Welsh and Chatterley, 1985). Previous floristic studies have been conducted in San Rafael Swell (Harris, 1980) and the Henry Mountains (Neese, 1981); however, aside from classification of coniferous habitat types (Youngblood and Mauk, 1985), no community studies have been done in this region.
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7

Heil, Kenneth, Rich Fleming, J. Porter, and William Romme. "A Vegetation Study of Capitol Reef National Park." UW National Parks Service Research Station Annual Reports 11 (January 1, 1987): 25–29. http://dx.doi.org/10.13001/uwnpsrc.1987.2615.

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Capitol Reef National Park lies in a relatively unexplored region of southcentral Utah. The diversity in geology and the elevation gradient (3,500-9,000 feet) allows for diverse vegetation including endemic and rare taxa (Welsh and Chatterley, 1985). Previous floristic studies have been conducted in San Rafael Swell (Harris, 1980) and the Henry Mountains (Neese, 1981); however, aside from classification of coniferous habitat types (Youngblood and Mauk, 1985), no community studies have been done in this region.
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8

Heil, Kenneth, Rich Fleming, J. Porter, and William Romme. "A Vegetation Study of Capitol Reef National Park." UW National Parks Service Research Station Annual Reports 12 (January 1, 1988): 51–57. http://dx.doi.org/10.13001/uwnpsrc.1988.2697.

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Capitol Reef National Park lies in a relatively unexplored region of southcentral Utah. The diversity in geology and the elevation gradient (3,500-9,000 feet) allows for diverse vegetation including endemic and rare taxa (Welsh and Chatterley 1985). Previous floristic studies have been conducted in San Rafael Swell (Harris 1980) and the Henry Mountains (Neese 1981); however, aside from classification of coniferous habitat types (Youngblood and Mauk 1985), no community studies have been done in this region.
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9

Johnson, Kaj M., and Arvid M. Johnson. "Localization of layer-parallel faults in San Rafael swell, Utah and other monoclinal folds." Journal of Structural Geology 22, no. 10 (2000): 1455–68. http://dx.doi.org/10.1016/s0191-8141(00)00046-8.

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10

Braathen, Alvar, Elizabeth Petrie, Tonje Nystuen, et al. "Interaction of deformation bands and fractures during progressive strain in monocline - San Rafael Swell, Central Utah, USA." Journal of Structural Geology 141 (December 2020): 104219. http://dx.doi.org/10.1016/j.jsg.2020.104219.

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11

Neuhauser, K. R. "Sevier-age ramp-style thrust faults at Cedar Mountain, northwestern San Rafael swell (Colorado Plateau), Emery County, Utah." Geology 16, no. 4 (1988): 299. http://dx.doi.org/10.1130/0091-7613(1988)016<0299:sarstf>2.3.co;2.

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12

Hunt-Foster, ReBecca, Martin Lockley, Andrew Milner, et al. "Tracking dinosaurs in BLM canyon country, Utah." Geology of the Intermountain West 3 (January 1, 2016): 67–100. http://dx.doi.org/10.31711/giw.v3.pp67-100.

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Although only recognized as a discrete stratigraphic unit since 1944, the Cedar Mountain Formation represents tens of millions of years of geological and biological history on the central Colorado Plateau. This field guide represents an attempt to pull together the results of recent research on the lithostratigraphy, chronostratigraphy, sequence stratigraphy, chemostratigraphy, and biostratigraphy of these medial Mesozoic strata that document the dynamic and complex geological history of this region. Additionally, these data provide a framework by which to examine the history of terrestrial fa
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13

Hunt-Foster, ReBecca K., Martin G. Lockley, Andrew R. C. Milner, et al. "Tracking dinosaurs in BLM canyon country, Utah." Geology of the Intermountain West 3 (May 26, 2018): 67–100. http://dx.doi.org/10.31711/giw.v3i0.8.

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Although only recognized as a discrete stratigraphic unit since 1944, the Cedar Mountain Formation represents tens of millions of years of geological and biological history on the central Colorado Plateau. This field guide represents an attempt to pull together the results of recent research on the lithostratigraphy, chronostratigraphy, sequence stratigraphy, chemostratigraphy, and biostratigraphy of these medial Mesozoic strata that document the dynamic and complex geological history of this region. Additionally, these data provide a framework by which to examine the history of terrestrial fa
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14

Richardson, J. A., C. B. Connor, P. H. Wetmore, L. J. Connor, and E. A. Gallant. "Role of sills in the development of volcanic fields: Insights from lidar mapping surveys of the San Rafael Swell, Utah." Geology 43, no. 11 (2015): 1023–26. http://dx.doi.org/10.1130/g37094.1.

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15

Kirkland, James, Marina Suarez, Celina Suarez, and ReBecca Hunt-Foster. "The Lower Cretaceous in east-central Utah—The Cedar Mountain Formation and its bounding strata." Geology of the Intermountain West 3 (January 1, 2016): 101–228. http://dx.doi.org/10.31711/giw.v3.pp101-228.

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Although only recognized as a discrete stratigraphic unit since 1944, the Cedar Mountain Formation represents tens of millions of years of geological and biological history on the central Colorado Plateau. This field guide represents an attempt to pull together the results of recent research on the lithostratigraphy, chronostratigraphy, sequence stratigraphy, chemostratigraphy, and biostratigraphy of these medial Mesozoic strata that document the dynamic and complex geological history of this region. Additionally, these data provide a framework by which to examine the history of terrestrial fa
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16

Kirkland, James I., Marina Suarez, Celina Suarez, and ReBecca Hunt-Foster. "The Lower Cretaceous in east-central Utah—The Cedar Mountain Formation and its bounding strata." Geology of the Intermountain West 3 (May 26, 2016): 101–228. http://dx.doi.org/10.31711/giw.v3i0.9.

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Although only recognized as a discrete stratigraphic unit since 1944, the Cedar Mountain Formation represents tens of millions of years of geological and biological history on the central Colorado Plateau. This field guide represents an attempt to pull together the results of recent research on the lithostratigraphy, chronostratigraphy, sequence stratigraphy, chemostratigraphy, and biostratigraphy of these medial Mesozoic strata that document the dynamic and complex geological history of this region. Additionally, these data provide a framework by which to examine the history of terrestrial fa
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17

JEFFERY, D. L., J. L. BERTOG, and J. R. BISHOP. "SEQUENCE STRATIGRAPHY OF DINOSAUR LAKE: SMALL SCALE FLUVIO-DELTAIC STRATAL RELATIONSHIPS OF A DINOSAUR ACCUMULATION AT THE AARON SCOTT QUARRY, MORRISON FORMATION, SAN RAFAEL SWELL, UTAH." PALAIOS 26, no. 5 (2011): 275–83. http://dx.doi.org/10.2110/palo.2010.p10-104r.

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18

Martz, Jeffrey, James Kirkland, Andrew Milner, William Parker, and Vincent Santucci. "Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah." Geology of the Intermountain West 4 (April 21, 2017): 99–180. http://dx.doi.org/10.31711/giw.v4.pp99-180.

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The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken d
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19

Martz, Jeffrey W., James I. Kirkland, Andrew R. C. Milner, William G. Parker, and Vincent L. Santucci. "Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah." Geology of the Intermountain West 4 (August 2, 2017): 99–180. http://dx.doi.org/10.31711/giw.v4i0.13.

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The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken d
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20

Potter-McIntyre, S., J. Allen, S. Y. Lee, W. S. Han, M. Chan, and B. McPherson. "Iron precipitation in a natural CO2reservoir: Jurassic Navajo Sandstone in the northern San Rafael Swell, UT, USA." Geofluids 13, no. 1 (2013): 82–92. http://dx.doi.org/10.1111/gfl.12014.

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21

Hilliard, Lyra. "Struggle over Utah’s San Rafael Swell: Wilderness, National Conservation Areas, and National Monuments by Jeffrey O. Durrant." Western American Literature 43, no. 3 (2008): 333–34. http://dx.doi.org/10.1353/wal.2008.0057.

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22

Zuluaga, Luisa F., Haakon Fossen, and Atle Rotevatn. "Progressive evolution of deformation band populations during Laramide fault-propagation folding: Navajo Sandstone, San Rafael monocline, Utah, U.S.A." Journal of Structural Geology 68 (November 2014): 66–81. http://dx.doi.org/10.1016/j.jsg.2014.09.008.

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23

Díez, M., C. B. Connor, S. E. Kruse, L. Connor, and I. P. Savov. "Evidence of small-volume igneous diapirism in the shallow crust of the Colorado Plateau, San Rafael Desert, Utah." Lithosphere 1, no. 6 (2009): 328–36. http://dx.doi.org/10.1130/l61.1.

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24

Kiyosugi, Koji, Charles B. Connor, Paul H. Wetmore, et al. "Relationship between dike and volcanic conduit distribution in a highly eroded monogenetic volcanic field: San Rafael, Utah, USA." Geology 40, no. 8 (2012): 695–98. http://dx.doi.org/10.1130/g33074.1.

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25

Bottcher, Jared L., Timothy E. Walsworth, Gary P. Thiede, Phaedra Budy, and David W. Speas. "Frequent Usage of Tributaries by the Endangered Fishes of the Upper Colorado River Basin: Observations from the San Rafael River, Utah." North American Journal of Fisheries Management 33, no. 3 (2013): 585–94. http://dx.doi.org/10.1080/02755947.2013.785993.

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26

Zuluaga, Luisa F., Atle Rotevatn, Eirik Keilegavlen, and Haakon Fossen. "The effect of deformation bands on simulated fluid flow within fault-propagation fold trap types: Lessons from the San Rafael monocline, Utah." AAPG Bulletin 100, no. 10 (2016): 1523–40. http://dx.doi.org/10.1306/04151614153.

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27

Fischer, Mark P., and Ryan D. Christensen. "Insights into the growth of basement uplifts deduced from a study of fracture systems in the San Rafael monocline, east central Utah." Tectonics 23, no. 1 (2004): n/a. http://dx.doi.org/10.1029/2002tc001470.

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28

Kirkland, James, Donald DeBlieux, ReBecca Hunt-Foster, John Foster, Kelli Trujillo, and Emily Finzel. "The Morrison Formation and its bounding strata on the western side of the Blanding basin, San Juan County, Utah." Geology of the Intermountain West 7 (June 4, 2020): 137–95. http://dx.doi.org/10.31711/giw.v7.pp137-195.

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In 2016 and 2017, the Utah Geological Survey partnered with the U.S. Bureau of Land Management to conduct a paleontological inventory of the Morrison Formation south and west of Blanding, Utah, along the eastern margin of the Bears Ears National Monument. The Morrison in this region is critical to understanding Upper Jurassic stratigraphy across the Colorado Plateau because it is the type area for the Bluff Sandstone, Recapture, Westwater Canyon, and Brushy Basin Members of the Morrison Formation, which are the basis for nomenclature in New Mexico and Arizona as well. Researchers have disagree
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29

Keller, Daniel L., Brian G. Laub, Paul Birdsey, and David J. Dean. "Effects of Flooding and Tamarisk Removal on Habitat for Sensitive Fish Species in the San Rafael River, Utah: Implications for Fish Habitat Enhancement and Future Restoration Efforts." Environmental Management 54, no. 3 (2014): 465–78. http://dx.doi.org/10.1007/s00267-014-0318-7.

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30

Stephens, Tara L., Richard J. Walker, David Healy, Alodie Bubeck, and Richard W. England. "Mechanical models to estimate the paleostress state from igneous intrusions." Solid Earth 9, no. 4 (2018): 847–58. http://dx.doi.org/10.5194/se-9-847-2018.

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Abstract. Dikes and sills represent an important component of the deformation history in volcanic systems, but unlike dikes, sills are typically omitted from traditional paleostress analyses in tectonic studies. The emplacement of sheet intrusions is commonly associated with Mode I fracturing in a low deviatoric stress state, in which dilation is perpendicular to the fracture plane. Many natural examples of sills and dikes, however, are observed to accommodate minor shear offsets, in addition to a component of dilation. Here we present mechanical models for sills in the San Rafael subvolcanic
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31

GIBERT, JORDI M. DE, University of. "Abstract: Environmental Ichnostratigraphy of Shallow Marine Carbonates in the Jurassic Carmel Formation, San Rafael Swell, Central Utah." AAPG Bulletin 82 (1998). http://dx.doi.org/10.1306/00aa87ba-1730-11d7-8645000102c1865d.

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32

Kevin J. Thomas1, James P. Evans1,. "ABSTRACT: Stratigraphic and Structural Heterogeneities in Faulted Aeolian Sandstone from Borehole Geophysics and Cores, San Rafael Swell, Central Utah." AAPG Bulletin 85 (2001). http://dx.doi.org/10.1306/61eed21a-173e-11d7-8645000102c1865d.

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33

FISCHER, MARK P., Department of Geo. "Abstract: Structural and Stratigraphic Controls on Fracture System Architecture: An Example from the Carmel Formation of the San Rafael Swell, Utah." AAPG Bulletin 82 (1998). http://dx.doi.org/10.1306/00aa867a-1730-11d7-8645000102c1865d.

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34

Bertog, J., D. Jeffery, K. Coode, W. Hester, D. Robinson, and J. Bishop. "Taphonomic patterns of a dinosaur accumulation in a lacustrine delta system in the Jurassic Morrison Formation, San Rafael Swell, Utah, USA." Palaeontologia Electronica, 2014. http://dx.doi.org/10.26879/372.

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35

Ryan D. Christensen1, Mark P. Fisch. "Abstract: Timing, Distribution, and Controls on Fracture Systems in the San Rafael Swell, Utah: Implications for Fracturing in Laramide-Style Fault-Propagation Folds." AAPG Bulletin 84 (2000) (2000). http://dx.doi.org/10.1306/c9ebd30f-1735-11d7-8645000102c1865d.

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36

Walker, R. J., D. Healy, T. M. Kawanzaruwa, et al. "Igneous sills as a record of horizontal shortening: The San Rafael subvolcanic field, Utah." Geological Society of America Bulletin, April 7, 2017, B31671.1. http://dx.doi.org/10.1130/b31671.1.

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37

Germa, Aurelie, Danielle Koebli, Paul Wetmore, et al. "Crystallization and Segregation of Syenite in Shallow Mafic Sills: Insights from the San Rafael Subvolcanic Field, Utah." Journal of Petrology, October 3, 2020. http://dx.doi.org/10.1093/petrology/egaa092.

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Abstract Exposed plumbing systems provide important insight into crystallization and differentiation in shallow sills beneath volcanic fields. We use whole rock major element, trace element and radiogenic isotopic compositions, along with mineral geochemical data on 125 samples to examine the conditions of melt differentiation in shallow sills from the exposed 4-Ma-old San Rafael subvolcanic field (SRVF), Utah. The field consists of ∼2000 dikes, 12 sills and 63 well preserved volcanic conduits. Intrusive rocks consist of mainly fine-grained trachybasalts and coarse-grained syenites, which are
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38

HULEN, JEFFREY B., JAMES A. COLLIST. "Abstract: Hydrocarbons in Miocene Lamproite Dikes of the San Rafael Desert, Utah - Implications for Fault-Controlled Oil Migration and Accumulation in the Western Colorado Plateau." AAPG Bulletin 82 (1998). http://dx.doi.org/10.1306/00aa8ad0-1730-11d7-8645000102c1865d.

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