新疆库鲁克塔格地区晚古元古代兴地塔格群沉积特征及其碳同位素研究

收稿日期: 2009-10-14

修回日期: 2009-12-17

刊出日期: 2010-03-15

Sedimentation Characteristic and Carbon Isotope Composition in Late Paleoproterozoic Xingditage Group in Quruqtagh Region of Xinjiang, China

Received Date: 14 October 2009

Revised Date: 17 December 2009

Publish Date: 15 March 2010

摘要: 新疆库鲁克塔格地区兴地塔格群被认为是晚古元古代地层,该地层黑色云母石英片岩的铅同位素测年为2 063.28~2 321.4 Ma。通过对兴地塔格群辛格尔组白云石大理岩的碳同位素测定,其碳同位素分布在5.15‰~-0.79‰PDB,大部分数据为2‰PDB,明显不同于中元古代1 600~1 400 Ma时期的δ¹³Ccarb值处在0‰~1‰PDB特征。其与国内外同时期地层的碳同位素数据比较,特别是与华北长城系碳同位素特征比较,认为辛格尔组应该属于晚古元古代1 700~1 600 Ma时期沉积产物。同时,对兴地塔格群的沉积地层特征及沉积环境进行系统研究,认为兴地塔格群沉积环境属于浅海沉积环境。
- 碳同位素 /
- 沉积环境 /
- 辛格尔组 /
- 晚古元古代 /
- 库鲁克塔格 /
- 新疆
Abstract: The Xingditage Group in the Quruqtagh region of Xinjiang is considered as the Late Paleoproterozoic stratigrap by whose age is 2063.28Ma to 2321.4Ma from Pb isotopic dating. The carbon isotopic composition of marble of the Xinge'er Formation of Xingditage Group shows that its carbon iso topic composition ranges from 5.15‰ PDB to-0.79‰ PDB,and most carbon isotopic data distribute In 2‰ PDB,much different from δ¹³C carb composition (0‰~1‰ PDB)in early Middle Proterozoic(1 600 ~1 400Ma).
- carbon isotope /
- sedimentary environment /
- Xinge’er Formation /
- Late Paleoproterozoic /
- Quruqtagh region /
- Xinjiang