Welcome to visit Geoscience!

Geoscience ›› 2018, Vol. 32 ›› Issue (02): 329-334.DOI: 10.19657/j.geoscience.1000-8527.2018.02.11

• Petrology • Previous Articles     Next Articles

Zircon U-Pb Ages and Geological Significance of Volcanic Rocks from Maoniushan Formation in the Northern Margin of Qaidam Basin

ZHANG Yaoling1,2(), NI Jinyu3, SHEN Yanxu4, WANG Chaoqun2, GAO Wanli2, HU Daogong2   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
    2. Institute of Geomechanics, Chinese Academy of Geoscience, Beijing 100081, China
    3. Minmetals Exploration and Development Co.Ltd., China Minmetals Corporation,Beijing 100010, China
    4. Cores and Samples Center of Land & Resources, Langfang,Hebei 065201, China
  • Received:2017-07-23 Revised:2017-12-01 Online:2018-04-10 Published:2018-05-07

Abstract:

The molasses of Maoniushan Formation rest unconformably on pre-Devonian strata and record the closure time of the Early Paleozoic ocean in the northern margin of Qaidam Basin. This research determinates zircon U-Pb isotopes from two rhyolite-tuff samples of volcanic rock member of upper Maomiushan Formation of Maoniushan mountain, northern margin of Qaidam Basin. The weighted mean 206Pb/238U ages of magmatic zircons from two samples are (396.5±2.4) Ma(n=17,MSWD=3.3)and (395.8±1.2) Ma(n=20,MSWD=1.1), interpreted as the formation time of the volcanic rocks. Combining past dating results about Maoniushan Formation of East Kunlun orogenic belt, we concluded that the formation time of the Maoniushan Formation around Qaidam Basin should be Late Silurian to Late Devonian, and the Caledonian movement of East Kunlun and northern margin of Qaidam Basin ended before Early Devonian instead of Late Devonian, as traditional thought.

Key words: Maoniushan Formation, volcanic rock, zircon U-Pb age, Devonian, Northern Qaidam Basin

CLC Number: