The geological development of the southern part of the New England Fold Belt
作者:
E. C. Leitch,
期刊:
Journal of the Geological Society of Australia
(Taylor Available online 1974)
卷期:
Volume 21,
issue 2
页码: 133-156
ISSN:0016-7614
年代: 1974
DOI:10.1080/00167617408728840
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
Two major divisions of the New England Fold Belt, Zone A and Zone B, are separated by the Peel Fault. Deposition in these two zones was probably contemporaneous (Lower Palaeozoic ‐ Lower Permian). Terminal orogenesis in both zones was also contemporaneous (Middle Permian) but whereas in Zone A deformation was only moderate, metamorphism was of burial type, and granitic emplacement was uncommon, in Zone B many rocks were severely deformed and regionally metamorphosed, and both syn‐tectonic and post‐tectonic granites are widespread.
点击下载:
PDF (1932KB)
返 回