摘要
首次在唐古拉地区晚二叠世—早三叠世拉卜查日组中获得牙形石化石,其分子为Hindeodus typicalis、H.eurypyge和H.praeparvus。根据其地层意义并结合层序地层学及海平面变化研究,最终将研究区二叠系与三叠系界线的可能位置定在实测剖面的29层顶、30层底。基于此,作者系统测试了拉卜查日组中的碳酸盐岩87Sr/86Sr比值,结果表明,二叠系/三叠系界线附近87Sr/86Sr比值为0.707017~0.707032,显著小于国内外其他地区二叠系/三叠系界线附近87Sr/86Sr比值。造成这种差异的主要原因,可能是由于唐古拉地区二叠系/三叠系界线附近存在广泛的火山活动以及上扬子地区二叠纪广泛的玄武岩喷发等地方性事件。此外,剖面上锶同位素演化曲线与海平面变化曲线对比显示,87Sr/86Sr比值的最小值与初始海泛面基本一致,锶同位素演化曲线与海平面变化曲线有着很好的一致性,说明全球海平面变化是其最主要的控制因素。
Conodont fossils were found for the first time in the Late Permian Labuchari Formation in the Tanggula Range. Theconodonts include Hindeodus typicalis, H. eurypyge and H. praeparvus. According to their significance and the investigation ofsequence stratigraphy and sea- level changes, the Permian /Triassic boundary may be determined between the top of 29 and thebottom of 30 of the measured section. Here, the carbonatite 87Sr/86Sr ratios of Labuchari Formation were determined. At the Permian/ Triassic boundary, 87Sr / 86 Sr ratios are from 0.707017 to 0.707032, which are significantly lower than those in other areas. The main
reasons for the remarkable difference might be the existence of extensive volcanic activities in Tangula Range at the Permian/
Triassic boundary and the basalt eruptions in Yangtze region during the late Permian. In addition, the comparison between the
strontium isotope curve and sea-level curve shows that the minimum 87Sr/86Sr ratio has a good consistency with the data of the first
flooding surface, suggesting that global sea level change was the main factors controlling the strontium isotope.
出处
《中国地质》
CAS
CSCD
北大核心
2016年第4期1139-1148,共10页
Geology in China
基金
国家自然科学基金项目(41101073
40872084)
中国地质调查局项目(12120113028800)联合资助~~
关键词
唐古拉地区
拉卜查日组
锶同位素
牙形石
相对海平面变化
Tangula Range
Labuchari Formation
strontium isotope
conodont
corresponding sea level change
