摘要:

Pillow lava structures are found in the supracrustals south of Tjörn, south-western Sweden. The pillow lava grades into banded amphibolites, mostly with rapidly changing composition and some intermediate and acid intercalations. These amphibolites are part of the Stora Le-Marstrand formation, which is dominated by greywackes. Both pillow lavas and ordinary supracrustals are metamorphosed before the intrusion of the 1650 Ma Rönnäng tonalite. An island are continental margin environment of formation is suggested.

ISSN:0016-786X    

DOI:10.1080/11035898409454617

出版商:Taylor & Francis Group    

年代:1984

数据来源: Taylor

ISSN:0016-786X    

DOI:10.1080/11035898409454618

出版商:Taylor & Francis Group    

年代:1984

数据来源: Taylor

摘要:

This is a scanned image of the original Editorial Board page(s) for this issue

ISSN:0016-786X    

DOI:10.1080/11035898409454596

出版商:Taylor & Francis Group    

年代:1984

数据来源: Taylor