TY - JOUR
T1 - Imbrication of a reference section
T2 - re-evaluation of the Adaminaby Beds at El Paso, Dalgety, New South Wales
AU - Glen, R. A.
AU - Stewart, I.
AU - Vandenberg, A. H. M.
PY - 1990
Y1 - 1990
N2 - Re-examination of a reference section through the Adaminaby beds at El Paso, west of Dalgety in southern New South Wales, does not support the conventionally held belief that rocks here form a simple Upper Ordovician homoclinal sequence which dips and youngs to the west. Rather, there has been thrust interleaving of a Lower Ordovician turbidite-chert sequence with an Upper Ordovician black shale sequence. The El Paso area thus lies in a thin-skinned thrust belt which was first recognized in the Delegate area 60 km to the south and which also extends north and east of Dalgety. -from Authors
AB - Re-examination of a reference section through the Adaminaby beds at El Paso, west of Dalgety in southern New South Wales, does not support the conventionally held belief that rocks here form a simple Upper Ordovician homoclinal sequence which dips and youngs to the west. Rather, there has been thrust interleaving of a Lower Ordovician turbidite-chert sequence with an Upper Ordovician black shale sequence. The El Paso area thus lies in a thin-skinned thrust belt which was first recognized in the Delegate area 60 km to the south and which also extends north and east of Dalgety. -from Authors
UR - http://www.scopus.com/inward/record.url?scp=0025526719&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0025526719
SN - 0035-9173
VL - 123
SP - 15
EP - 26
JO - Journal & Proceedings - Royal Society of New South Wales
JF - Journal & Proceedings - Royal Society of New South Wales
IS - 1-2
ER -