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青藏高原北部古近系新建岩石地层单位——祖尔肯乌拉山组
Jurhen Ul Formation—a new Paleogene lithostratigraphic unit in the northern Qinghai-Tibet Plateau
【摘要】 将青藏高原北部祖尔肯乌拉山一带,广泛分布的一套近水平熔岩被状产出的、同位素年龄为古近纪始新世中晚期的中酸性熔岩(岩性主要为安粗岩、粗面岩、橄榄玄粗岩夹火山角砾岩),新建为正式组级岩石地层单位祖尔肯乌拉山组,指定了正层型和副层型剖面,并进行了详细描述。
【Abstract】 A sequence of subhorizontal intermediate-acid lavas is widespread in the Jurhen Ul Mountain area of the northern Qinghai-Tibet Plateau.It is composed mainly of latite,trachyte and shoshonite with volcanic breccia.Isotopic age determination shows that these volcanic rocks are of mid-late Eocene age.This sequence of lavas is attributed to a new established formal lithostratigraphic unit called the Jurhen Ul Formation in this paper.The holostratotype and parastratotype sections of the Jurhen Ul Formation are as-signed and described in detail.
【关键词】 青藏高原;
祖尔肯乌拉山组;
始新世;
火山岩;
岩石地层;
【Key words】 Qinghai-Tibet Plateau; Jurhen Ul Formation; Eocene; volcanic rock; lithostratigraphy;
【Key words】 Qinghai-Tibet Plateau; Jurhen Ul Formation; Eocene; volcanic rock; lithostratigraphy;
【基金】 中国地质调查局1∶25万乌兰乌拉湖幅区域地质调查项目成果。
- 【文献出处】 地质通报 ,Regional Geology of China , 编辑部邮箱 ,2003年Z1期
- 【分类号】P534
- 【被引频次】3
- 【下载频次】97