Canal de las Ballenas Group

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Series: GSA Special Papers
Published: 01 January 1993
DOI: 10.1130/SPE279-p61
... named the Canal de Las Ballenas Group. Conodont fragments and favositid corals indicate a Devonian age, suggesting correlation with rocks in the Sierra Las Pinta to the northwest, and to southern Sonora to the east. The recognition of these rocks adds an important link to our understanding...
Journal Article
Published: 01 December 2011
Bulletin of the Seismological Society of America (2011) 101 (6): 3072-3080.
...-Vertti A. Mendoza A. ( 2011 ). The August 3, 2009 Canal de Ballenas region, Gulf of California earthquake ( M w  6.9) and its aftershocks , Bull. Seismol. Soc. Am. , 101 , 929 - 939 . Fielding E. J. LePrince S. Wei S. Sladen A. Simons M. Avouac J. P. Lohman...
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Journal Article
Published: 14 February 2018
Seismological Research Letters (2018) 89 (2A): 338-344.
...: the first near the East Pacific Rise, the second at the Canal de Ballenas transform fault in central GoC, and the third in the Cerro Prieto geothermal field in the northern gulf. Di Luccio et al. (2014) also identify an asthenospheric window in the north‐central region ( ∼ 28 °  N) characterized...
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Series: Memoir - AAPG
Published: 01 January 2001
DOI: 10.1306/M75768C12
EISBN: 9781629810638
..., and the Sierra Madre terrane comprises Triassic strata of La Ballena Formation ( Silva-Romo, 1993 ) in the Sierra de Salinas and Charcas. We concur with Monod and Calvet, who assign an early Cretaceous age for pillow lava and limestone in the vicinity of Zacatecas city, which may be correlative with the Chilitos...
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Journal Article
Journal: Paleobiology
Published: 01 February 2009
Paleobiology (2009) 35 (1): 77-93.
... differences in comparative diversity and abundance among major ecological groups of scallops. Free-swimming scallops constituted the most diverse guild throughout most of the last 10 Myr in the SWC, and were always moderately to very abundant. Leptopecten and Argopecten were also highly diverse throughout...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.255.01.13
EISBN: 9781862395039
.... Bryozoan-dominated regions are located around the southern tip of Isla Coronado to Canal de Ballenas and south of Isla La Ventana (Fig. 6 ). This bryozoan-rich belt ranging from 20–110 m water depth coincides with areas of high percentages of coarse sediments. In the gravel size fraction, up to 80...
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Journal Article
Published: 02 December 2014
Bulletin of the Seismological Society of America (2015) 105 (1): 431-444.
... for these differences, we regressed the absolute errors shown in Figure  6a against PDS twice, each time with a different grouping. We first grouped the values by their station code (e.g., B084) and then by their channel code (e.g., CH0). For example, in the station‐grouped regression, we regress all offsets...
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Journal Article
Published: 01 August 2001
Bulletin of the Seismological Society of America (2001) 91 (4): 781-791.
... Island, located to the southeast of the Lower Delfin Basin, is bounded by the Canal de Ballenas, a transform fault on the southwest and the abandoned Tiburon transform fault on the northeast ( Lonsdale, 1989 ). This region lies within the Gulf of California extensional province (see Fig. 1...
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