冀北滦平地区中生代火山岩地层锆石U-Pb测年及启示

张宏; 袁洪林; 胡兆初; 柳小明; 第五春荣

Volume 30 Issue 6

Jun. 2005

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Article Navigation > Earth Science > 2005 > 30(6): 707-720

ZHANG Hong, YUAN Hong-lin, HU Zhao-chu, LIU Xiao-ming, DIWU Chun-rong, 2005. U-Pb Zircon Dating of the Mesozoic Volcanic Strata in Luanping of North Hebei and Its Significance. Earth Science, 30(6): 707-720.

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U-Pb Zircon Dating of the Mesozoic Volcanic Strata in Luanping of North Hebei and Its Significance

1.
Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
2.
Shenyang Institute of Geology and Mineral Resources, China Geological Survey, Shenyang 110032, China

Received Date: 2005-06-21
Publish Date: 2005-11-25

Abstract

Abstract

The Mesozoic strata in Luanping, North Hebei Province are the most complete in North Hebei-West Liaoning, and the Luanping area is the only area where the deposit action in the Late Mesozoic is successive. A lot of researchers think the boundary of the J₃-K₁ and the tectonic framework transition interface in Mesozoic Era in North Hebei-West Liaoning are located between the Tuchengzi and Zhangiiakou formations in the Luanping area. The Mesozoic strata in Luanping from the lower to the upper are the Tiaojishan Formation, Tuehengzi Formation, Zhangjiakou Formation, Dabeigou Formation, Dadianzi Formation and the Xiguayuan Formation. U-Pb zircon dating of LA-ICP-MS obtained the age frame of the Mesozoic volcanic strata in the Luanping area. The top age of the Tiaojishan Formation is (162.8±3.2)Ma, the main forming period of the Tuehengzi Formation is (142.6±1.3)Ma-(136.4±1.9)Ma, the forming period of the Zhangjiakou Formation is (135.7±1.8)Ma--(135.2±2.3)Ma, and the age of the volcanic rocks in the top of the Dadianzi Formation is (131.4±3. 7)Ma--(130.2±3. 0)Ma. Analysis shows that the rare earth element characteristics of zircons from the Tuehengzi Formation are very similar to those from the Zhangiiakou Formation, but are very different from those from the Tiaojishan Formarion. Combined with the field characteristics of the strata, the following conclusions are drawn: (1) the time interval Detween the Tuchengzi and Tiaojishan formations is longer, and the magmatic sources of the volcanic rocks are very different; the forming period between the Tuchengzi and the Zhangjiakou formations is continuous, and the magmatic sources of the volcanic rocks are very similar. The results imply that the Tuchengzi and Zhangjiakou formations were formed in the same geological background, and so are not the boundary of the J₃-K₁ and the tectonic framework transition interface between the Tuchengzi and Zhangjiakou formations in the Luanping area. (2) The age of the volcanic rocks in the top of the Dadianzi Formation corresponds to that of the bottom of the Yixian Formation in the Beipiao-Yixian area in West Liaoning Province, and corresponds to that of the top of the Zhangiiakou Formation in Lingyuan, West Liaoning Province.
- Mesozoic strata,
- zircon,
- LA-ICP-MS U-Pb dating,
- rare earth element,
- J₃-K₁ boundary,
- tectonic framework transition interface,
- Luanping area

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