1988
DOI: 10.1130/0091-7613(1988)016<0692:aasiso>2.3.co;2
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Age and Sr isotopic signature of the Catoctin volcanic province: Implications for subcrustal mantle evolution

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Cited by 92 publications
(53 citation statements)
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“…Most workers now agree that the Catoctin Formation is Late Proterozoic in age, based on isotopic dating (Rankin and others, 1969;Badger and Sinha, 1988;see Catoctin Formation below) , and that the fossiliferous Antietam Quartzite is Early Cambrian in age (Hesser, 1938, p.4-6) . Because of their lack of fossils , the Harpers Formation, Weverton Quartzite, and Loudoun Formation have been arbitrarily referred by some workers to the Precambrian (for example, Hesser, 1938;Mitra, 1989) or have been assigned a Cambrian(?)…”
Section: Age and Thickness Assignmentsmentioning
confidence: 99%
“…Most workers now agree that the Catoctin Formation is Late Proterozoic in age, based on isotopic dating (Rankin and others, 1969;Badger and Sinha, 1988;see Catoctin Formation below) , and that the fossiliferous Antietam Quartzite is Early Cambrian in age (Hesser, 1938, p.4-6) . Because of their lack of fossils , the Harpers Formation, Weverton Quartzite, and Loudoun Formation have been arbitrarily referred by some workers to the Precambrian (for example, Hesser, 1938;Mitra, 1989) or have been assigned a Cambrian(?)…”
Section: Age and Thickness Assignmentsmentioning
confidence: 99%
“…The entire area of Shaver Hollow is underlain by granitic rocks of Grenville (1.0-1.1 Ga) age, intruded by small dikes related to the Catoctin metavolcanic rocks of 570 ma (Badger and Sinha, 1988). These granitic rocks were first recognized by Jonas (1935), who identified them as hypersthene granodiorites.…”
Section: Bedrock Geologymentioning
confidence: 99%
“…More recent work by Badger and Sinha (1988) and Badger (1993) established the age of the Catoctin at 570 ma and provided new information on the chemistry and origin of these rocks. The chemistry of these rocks is least altered in the dikes, is typical of tholeiite basalts with moderately high titanium content, and is similar to the chemistry of large, extensive plateau basalts.…”
Section: Bedrock Geologymentioning
confidence: 99%
“…This magmatism is contemporaneous with a second pulse of bimodal magmatism throughout the Appalachians (e.g. Badger and Sinha, 1988;Rankin et al, 1989;Aleinikoff et al, 1995) and related to continental break-up in Laurentia (Cawood et al, 2001 Pringle, 1940;Tanner, 1995 Provenance studies summarised here (Fig. 7;Cawood et al, 2003Cawood et al, , 2004 provide useful data that track the evolution and denudation history of the hinterland.…”
Section: The Pre-dalradian Basementmentioning
confidence: 99%