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Agua Fria Formation

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Series: GCSSEPM
Published: 01 July 1993
DOI: 10.5724/gcs.92.13.0143
EISBN: 978-0-9836097-3-5
...ABSTRACT ABSTRACT Geologic mapping on the Chortís block has defined two major Mesozoic units which are older than the well-known, lower Cretaceous Yojoa Group. The two units have been considered part of the same stratigraphic element, the Honduras Group. The Agua Fría Formation, a dominantly...
FIGURES | View All (8)
Image
—Ahuas area showing seismic lines, Patuca subsurface fault system, Sixatign...
Published: 11 October 1996
Figure 5 —Ahuas area showing seismic lines, Patuca subsurface fault system, Sixatigni hills composed of Honduras Group clastics (Jhg), Yojoa Group limestones (Ky), and Ilama conglomerates (Ki), and low hills of Agua Fria Formation (Jaf) that may be related to faults. Note airstrips at Ahuas.
Image
—Tectonic map of Patuca region, Mosquitia basin. Ti = Tertiary intrusive, T...
Published: 11 October 1996
Honduras Group, Jaf = Middle Jurassic Agua Fria Formation, Pm = Paleozoic metamorphics, long dashed lines = surface faults, short dashed lines = subsurface faults (Ahuas block).
Image
—Stratigraphic summary of Embarcadero 1 and Raiti-Tara 1 wells. Ta = Ahuas ...
Published: 11 October 1996
limestone and quartz conglomerates, Jr = Rio Ribra beds, which are hard, dense, fine-grained red beds, Jaf = Agua Fria Formation, which is hard, dense, fine-grained dark clastics and low-grade dark-gray phyllite.
Image
Figure 1. A: Tectonic location of southern Mexico (SM) and Chortís block (...
Published: 01 January 2008
Formation (tf), accumulated to the northwest of the Guayape-Papalutla fault system (GPFS). Connection between the Tecocoyunca Group (tg) and Agua Fria Formation (aff), both Middle Jurassic clastic units, appears to the southeast. Southern Mexico ( Campa and Coney, 1983 ): TMVB—Transmexican Volcanic Belt
Image
—Regional geology of Honduras and northern Nicaragua after  Dengo et al. (1...
Published: 11 October 1996
Figure 6 —Regional geology of Honduras and northern Nicaragua after Dengo et al. (1969) , Mills and Hugh (1974) , and Kozuch (1991) . Exploratory dry holes total depths in meters. Jaf = Middle Jurassic Agua Fria Formation, Ky = Lower Cretaceous Yojoa Group, Ki = Cretaceous intrusive, KTi
Journal Article
Journal: AAPG Bulletin
Published: 11 October 1996
AAPG Bulletin (1996) 80 (10): 1627–1640.
...Figure 5 —Ahuas area showing seismic lines, Patuca subsurface fault system, Sixatigni hills composed of Honduras Group clastics (Jhg), Yojoa Group limestones (Ky), and Ilama conglomerates (Ki), and low hills of Agua Fria Formation (Jaf) that may be related to faults. Note airstrips at Ahuas. ...
FIGURES | View All (15)
Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2428(06)
... (1991) proposed ∼50 km of left-lateral motion based in part on the apparent lateral offset of the Agua Fria Formation on either side of the fault. The map compilation shown in Figure 2 indicates that the apparent left-lateral offset is closer to 60 km (length of line indicated by “1” in Fig. 2...
Series: GCSSEPM
Published: 01 December 2007
DOI: 10.5724/gcs.07.27.0273
EISBN: 978-0-9836096-3-6
..., (2) Coyula, (3) Agua Fria, (4) Coapechaca, (5) Tajin, and (6) Presidente Alemán. The Acatepec outcrop is located at the northwest end of cross-section A-A’, west of the pueblo of Chicontepec. Hydrocarbon shows were documented in the Chicontepec Formation as early as 1926, but it was not until...
Series: GSA Special Papers
Published: 01 April 2013
DOI: 10.1130/2013.2494(10)
... embayment of the Española Basin and the northern end of the Estancia Basin. The east limb of the syncline is cut by northerly trending, graben-forming, normal faults of the Agua Fria fault system in the Santa Fe embayment. East of the Tijeras-Cañoncito fault system, the east limb of the Estancia Basin...
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1987
DOI: 10.5382/GB.01
EISBN: 9781934969540
...Abstract Abstract 0.0 Bell Ranch northeast of Mayer, Arizona. Proceed on dirt road down the Agua Fria River. 0.9 Road leaves valley bottom and climbs to the south through metasedimentary rocks. 1.3 Road from the Binghampton and Copper Queen mines joins this road on the left. 2.7 Crossing...
Journal Article
Journal: GSA Bulletin
Published: 01 February 1953
GSA Bulletin (1953) 64 (2): 151–196.
...C GARDLEY MOON Abstract The 15-minute Agua Fria quadrangle in southwestern Brewster County, Texas, is arid, sparsely vegetated, and includes diverse topographic features that result chiefly from complex structure and variation in rock resistance to erosion. The mountainous and more complicated...
Journal Article
Journal: Palynology
Published: 03 July 2018
Palynology (2018) 42 (3): 420–433.
... ( Figure 1 ), about 400 km north of the Merced succession. We sampled the Raya and Agua Caliente formations, along the Aguas Frias Creek (−07°11′40.8901″, −074°57′37.8698″), a tributary of the Ucayali River. The Raya Formation is 138 m thick and it is mainly composed of white to yellow-brown ripple-cross...
Journal Article
Journal: Geology
Published: 01 January 2008
Geology (2008) 36 (1): 75–78.
... Formation (tf), accumulated to the northwest of the Guayape-Papalutla fault system (GPFS). Connection between the Tecocoyunca Group (tg) and Agua Fria Formation (aff), both Middle Jurassic clastic units, appears to the southeast. Southern Mexico ( Campa and Coney, 1983 ): TMVB—Transmexican Volcanic Belt...
FIGURES
Journal Article
Published: 01 May 2017
The Canadian Mineralogist (2017) 55 (3): 437–456.
... and intermediate rocks, forming enclaves in the granodiorites or locally small bodies. These rocks are intrusive in the greenstone belts and in the older tonalite–trondhjemite series and are crosscut by the Água Fria trondhjemite ( Leite et al . 2004 ). (2) A minor occurrence of younger tonalite–trondhjemite...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2000
GSA Bulletin (2000) 112 (11): 1650–1666.
... caused by rising relative sea level. At Agua Fria (location 3, Fig. 2 ) more than 150 m of Bathonian and lower Callovian sandstones (Gulisano and Gutierrez Pleimling, 1994) are capped by Tabanos Formation evaporites ( Fig. 10 ) equivalent to the evaporites at Chacay Melehue (location 1...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 2022
AAPG Bulletin (2022) 106 (3): 495–516.
... its porosity, becoming an excellent reservoir rock. In the Turonian, open waters prevailed and favored conditions for the deposition of shaly, organic-rich limestones of the Agua Nueva Formation. Younger Campanian and Maastrichtian units are more clay-rich, because this was a time when shale...
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Journal Article
Journal: SEG Discovery
Published: 01 April 1996
SEG Discovery (1996) (25): 1–14.
... Diablillos 12 Incahuasi 13 Río Blanco 14 Cerro Atajo 15 Bajo Del Durazno 16 Agua Tapada 17 Farallón Negro (Alto de La Blenda) 18 Bajo de La Alumbrera 19 Agua Rica 20 Capillitas 21 Laguna Verde 22 San Nicolás 23 King Tut 24 Famatina 25...
FIGURES
Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2428(05)
... of Japan (MMAJ), 1980 ; Kozuch, 1991 ) and Grenville-age orthogneiss ( Manton, 1996 ) (Fig. 2) . Basement of the Eastern Chortis terrane consists of Jurassic unmetamorphosed Agua Fria Formation strata overlying metamorphosed Agua Fria strata ( Gordon, 1993a ; Rogers, 1994 ; Rogers et al., Chapter 6...
Journal Article
Published: 16 August 2011
Geological Magazine (2012) 149 (2): 208–220.
... Atacama Fault System The sub-vertical shear zones are the most conspicuous structures in the Bahia Agua Dulce area and the focus of this study. The dominant mechanical anisotropy in the various rock units, i.e. bedding in the Arrayán, Huentelauquén and El Quereo formations ( Fig. 3 a) and the S2...