DISCOVERY OF THE EARLY JURASSIC VOLCANIC ROCKS IN XINLIN AREA OF NORTHERN DAXINGANLING MOUNTAINS: Geological Implication

LIU Tao; JI Feng; WANG Wen-dong; WANG Jiu-yi; ZHAO Xi-dong

doi:10.13686/j.cnki.dzyzy.2022.01.001

2022 Vol. 31, No. 1

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LIU Tao, JI Feng, WANG Wen-dong, WANG Jiu-yi, ZHAO Xi-dong. DISCOVERY OF THE EARLY JURASSIC VOLCANIC ROCKS IN XINLIN AREA OF NORTHERN DAXINGANLING MOUNTAINS: Geological Implication[J]. Geology and Resources, 2022, 31(1): 1-12. doi: 10.13686/j.cnki.dzyzy.2022.01.001

Citation:

LIU Tao, JI Feng, WANG Wen-dong, WANG Jiu-yi, ZHAO Xi-dong. DISCOVERY OF THE EARLY JURASSIC VOLCANIC ROCKS IN XINLIN AREA OF NORTHERN DAXINGANLING MOUNTAINS: Geological Implication[J]. Geology and Resources, 2022, 31(1): 1-12. doi: 10.13686/j.cnki.dzyzy.2022.01.001

DISCOVERY OF THE EARLY JURASSIC VOLCANIC ROCKS IN XINLIN AREA OF NORTHERN DAXINGANLING MOUNTAINS: Geological Implication

1.
Harbin Center of Comprehensive Natural Resources Survey, CGS, Harbin 150086, China
2.
No.3 Oil Production Plant Geological Institute of Daqing Oilfield Ltd., Co., Daqing 163000, Heilongjiang Province, China

Received Date: 09 August 2021

Revised Date: 15 October 2021

Publish Date: 25 February 2022

Abstract

Abstract

The Early Jurassic acid volcanic rocks are newly discovered in Zhanbeicun Formation of Xinlin area in northern Daxinganling Mountains, from which two samples of zircon LA-ICP-MS U-Pb ages are determined. The first is sericitized rhyolite, with the testing point deviating to the right side of concordant curve on the concordia diagram-a typical discordant age, yielding the intersecting age with concordant curve of 192.0±1 Ma(MSWD=1.2), which is the cooling crystallization age of rhyolites after extrusion. The second one is weakly silicified rhyolite with a concordant age of 178.0±1 Ma, which is the result of the loss of radioactive trace element Pb, and the rock-forming age should be close to that of the sericitized rhyolite. The volcanic rocks are petrochemically and geochemically characterized by high Ti rhyolite and I-type rhyolite. The Mg^# value of the rhyolite(0.43-0.73) and content of hypersthene in CIWP norm minerals (0.25%-0.96%) support that the rhyolite is derived from crystallization-differentiation of basic magma.
- Early Jurassic /
- rhyolite /
- zircon age /
- geochemistry /
- Daxinganling Mountains

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References

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