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Sangre de Cristo Formation

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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1959
AAPG Bulletin (1959) 43 (5): 1093–1094.
... of the geosyncline, and sediments of the overlying Sangre de Cristo formation of Pennsylvanian and Permian age were deposited as a predominantly non-marine suite which finally filled the geosyncline. During Laramide orogeny the troughal part of the geosyncline was elevated to form the Sangre de Cristo uplift...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2002
GSA Bulletin (2002) 114 (7): 804–828.
...Richard G. Hoy; Kenneth D. Ridgway Abstract Pennsylvanian–Permian synorogenic deposits (Minturn and Sangre de Cristo Formations) of the Central Colorado trough record an interplay of deformation and sedimentation in an Ancestral Rocky Mountains basin. The Central Colorado trough was a north...
FIGURES | View All (15)
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1960
AAPG Bulletin (1960) 44 (12): 1895–1902.
... to the Sangre de Cristo formation of Pennsylvanian and Permian age. Two units of probable Triassic age have been separated from the top of the Sangre de Cristo formation; one is here described and named the Johnson Gap formation. The other is correlated with the Lykins formation (Fenneman, 1905 , pp. 24–26...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1985
AAPG Bulletin (1985) 69 (5): 854.
...David A. Lindsey; Reino F. Clark; Sandra J. Soulliere ABSTRACT The Middle Pennsylvanian Minturn Formation and the Pennsylvanian and Permian Sangre de Cristo Formation of the northern Sangre de Cristo Range form a 4,000-m (13,000-ft) thick, progradational sequence of fan-delta and alluvial-fan...
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 1986
DOI: 10.1306/M41456C26
EISBN: 9781629811451
... Abstract The Middle Pennsylvania!) Minturn Formation and the Pennsylvanian-Permian Sangre de Cristo Formation of the northern Sangre de Cristo Range form a thick progradational sequence of coarse clastic sediments. These sediments were deposited along the western margin of the central Colorado...
Image
Figure 7. Measured sections of the <b>Sangre</b> <b>de</b> <b>Cristo</b> <b>Formation</b> along the wes...
Published: 01 July 2002
Figure 7. Measured sections of the Sangre de Cristo Formation along the western margin of the Central Colorado trough. See Figure 2 for lithologic patterns and Figure 3 for measured section locations. Arrows denote paleocurrent directions determined from imbricated clasts in conglomerate
Image
Figure 9. Measured section from the <b>Sangre</b> <b>de</b> <b>Cristo</b> <b>Formation</b> along the ea...
Published: 01 July 2002
Figure 9. Measured section from the Sangre de Cristo Formation along the eastern margin of the Central Colorado trough. See Figure 2 for lithologic patterns and Figure 3 for measured section location. Arrows denote paleocurrent directions measured from imbricated clasts in conglomerate and from
Image
—Depositional environment: Lower member of <b>Sangre</b> <b>de</b> <b>Cristo</b> <b>formation</b>.
Published: 01 August 1959
Fig. 11. —Depositional environment: Lower member of Sangre de Cristo formation.
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1956
AAPG Bulletin (1956) 40 (4): 786–787.
... and southeastern Colorado. The Uncompahgre was strongly uplifted along its east side and the ancient Apishapa Sierra Grande subsided to receive coarse arkosic clastics during late Pennsylvanian time. This writer believes the Sangre de Cristo formation in the Raton basin area is Missouri and Virgil in age...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1959
AAPG Bulletin (1959) 43 (8): 1896–1939.
...Fig. 11. —Depositional environment: Lower member of Sangre de Cristo formation. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 2041–2075.
... in the western half of the northern Raton basin where it may be 4,000 feet thick. Orogenic debris of the Sangre de Cristo Formation of Pennsylvanian and Early Permian age was derived mainly from the San Luis uplift, filled the Rowe-Mora and Central Colorado basins, and lapped onto Precambrian rocks of the other...
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Journal Article
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