摘要
准噶尔盆地西缘新发现的克拉玛依蛇绿混杂带,其形成时代尚未给出确切的结论。本文通过微体古生物研究,确定该蛇绿混杂岩带形成于早古生代。
The newly discovered Karamay ophiolitic mélange, distributing along the west edge of the Junggar basin, is of important to understand the tectonic of the western Junggar. However, no certain conclusion about the formation age of this mélange was reached. This paper reports the latest studies on microfossils, which demonstrated that the formation age of this ophiolitic mélange was Early Paleozoic.
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2007年第7期1573-1576,共4页
Acta Petrologica Sinica
基金
国家科技支持计划重点项目资助(批准号:2006BAB07B08)。