摘要
首次在藏北南羌塘坳陷地区中侏罗世晚期地层中发现硅化木,本文对硅化木的基本特征进行了描述,据同一层位中采集的大量孢粉及双壳类化石证明,该硅化木属中晚侏罗世。结合区域地质及含硅化木地层的沉积学特征分析表明,南羌塘坳陷地区中侏罗世晚期属干热-潮温气候,从而深化了对青藏高原中侏罗世晚期气候环境的认识。
Silicified wood happen to first one found within the beds of late middle Jurassic in depression region of Nanqiangtang, North Tibet, this paper describes basic features of the silicified wood, which is attributed to middle - upper Jurassic by plentiful evidences of rendoze and bivalve fossils collected from same horizon. Together with regional geology and sedimentary characteristic of the strata with silicified wood, the study shows the Nanqiangtang depression area of late - phase middle Jurassic is in hot - humid temperature, further strengthening the acknowledges for climate and environment of late middle Jurassic in Tibet Plateau.
出处
《贵州地质》
2007年第2期126-129,共4页
Guizhou Geology
基金
<青藏高原油气资源战略选区调查与评价>项目:羌塘盆地扎仁区块1:5万石油地质构造详查专题。科油[2006]02号
关键词
硅化木
中侏罗世
干热-潮湿气候
南羌塘坳陷
青藏高原
silicified wood
middle Jurassic
dry hot and humid climate
Nanqiangtang depression
Tibet Plateau