1966
DOI: 10.1021/ba-1966-0055.ch008
|View full text |Cite
|
Sign up to set email alerts
|

Analysis and Paragenetic History of Anthraxolite in Ordovician Slate, Eastern Pennsylvania

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
2
0

Year Published

1971
1971
1971
1971

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…However, the contention that the dominant mica is n illite ri (presumably 1M muscovite) is shown to be suspect. Further evidence for metamorphism in the Martinsburg is the occurrence of anthraxolite which Stevens (1966) showed is a metamorphic product, although he believed that the metamorphism occurred during the Taconic orogeny.…”
Section: Lithotectonic Unitmentioning
confidence: 99%
See 1 more Smart Citation
“…However, the contention that the dominant mica is n illite ri (presumably 1M muscovite) is shown to be suspect. Further evidence for metamorphism in the Martinsburg is the occurrence of anthraxolite which Stevens (1966) showed is a metamorphic product, although he believed that the metamorphism occurred during the Taconic orogeny.…”
Section: Lithotectonic Unitmentioning
confidence: 99%
“…The idea that the Martinsburg was severely cleaved during the Taconic orogeny led Stevens (1966) This proposed sequence is only a suggestion gleaned from the field data. Probably all events overlapped to some degree, and the order may have varied depending on local stress conditions.…”
mentioning
confidence: 99%