摘要:

Qureshi (1984) suggested that a dense mafic pile existed beneath the Sydney Basin. Since his regional separation leading to residual anomalies does not allow for the negative effects of regional granitoids, his residual values and interpretation were too positive. An alternative solution requires no huge unexplained or localized positive sources. Instead, the known materials of the Sydney Basin and Lachlan Fold Belt are sufficient to explain all presently defined features of the gravity field. The basement to the Sydney Basin is almost certainly an extension of the Lachlan Fold Belt as exposed at Bathurst or Goulburn.

ISSN:0812-0099    

DOI:10.1080/08120099008727910

出版商:Taylor & Francis Group    

年代:1990

数据来源: Taylor

ISSN:0812-0099    

DOI:10.1080/08120099008727911

出版商:Taylor & Francis Group    

年代:1990

数据来源: Taylor

ISSN:0812-0099    

DOI:10.1080/08120099008727912

出版商:Taylor & Francis Group    

年代:1990

数据来源: Taylor