Vitrinite reflectance anisotropy as a tectonic fabric element

James C. Hower; Alan Davis

doi:10.1130/0091-7613(1981)9<165:VRAAAT>2.0.CO;2

Vitrinite reflectance anisotropy as a tectonic fabric element

James C. Hower
, Alan Davis

Earth and Environmental Sciences

Producción científica: Article › revisión exhaustiva

57 Citas (Scopus)

Resumen

The anisotropy of the coal maceral vitrinite was analyzed in relation to the tectonic setting of a coal from the Southern Anthracite Field in Pennsylvania. For the coal studied, the maximum-intermediate reflectance plane essentially paralleled the axial plane of the synclinorium (N66°E strike, 64°SE dip).

Idioma original	English
Páginas (desde-hasta)	165-168
Número de páginas	4
Publicación	Geology
Volumen	9
N.º	4
DOI	https://doi.org/10.1130/0091-7613(1981)9<165:VRAAAT>2.0.CO;2
Estado	Published - 1981

ASJC Scopus subject areas

Geology

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title = "Vitrinite reflectance anisotropy as a tectonic fabric element",

abstract = "The anisotropy of the coal maceral vitrinite was analyzed in relation to the tectonic setting of a coal from the Southern Anthracite Field in Pennsylvania. For the coal studied, the maximum-intermediate reflectance plane essentially paralleled the axial plane of the synclinorium (N66°E strike, 64°SE dip).",

author = "Hower, \{James C.\} and Alan Davis",

year = "1981",

doi = "10.1130/0091-7613(1981)9<165:VRAAAT>2.0.CO;2",

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T1 - Vitrinite reflectance anisotropy as a tectonic fabric element

AU - Hower, James C.

AU - Davis, Alan

PY - 1981

Y1 - 1981

N2 - The anisotropy of the coal maceral vitrinite was analyzed in relation to the tectonic setting of a coal from the Southern Anthracite Field in Pennsylvania. For the coal studied, the maximum-intermediate reflectance plane essentially paralleled the axial plane of the synclinorium (N66°E strike, 64°SE dip).

AB - The anisotropy of the coal maceral vitrinite was analyzed in relation to the tectonic setting of a coal from the Southern Anthracite Field in Pennsylvania. For the coal studied, the maximum-intermediate reflectance plane essentially paralleled the axial plane of the synclinorium (N66°E strike, 64°SE dip).

UR - https://www.scopus.com/pages/publications/0001452078

UR - https://www.scopus.com/pages/publications/0001452078#tab=citedBy

U2 - 10.1130/0091-7613(1981)9<165:VRAAAT>2.0.CO;2

DO - 10.1130/0091-7613(1981)9<165:VRAAAT>2.0.CO;2

M3 - Article

AN - SCOPUS:0001452078

SN - 0091-7613

VL - 9

SP - 165

EP - 168

JO - Geology

JF - Geology

IS - 4

ER -

Vitrinite reflectance anisotropy as a tectonic fabric element

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