孙吴-嘉荫盆地晚白垩世地层物源及构造背景

贾啸宇; 高福红; 修铭; 刘国卿

doi:10.3799/dqkx.2020.252

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2379-2390

Jia Xiaoyu, Gao Fuhong, Xiu Ming, Liu Guoqing, 2021. Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin. Earth Science, 46(7): 2379-2390. doi: 10.3799/dqkx.2020.252

Citation:

Jia Xiaoyu, Gao Fuhong, Xiu Ming, Liu Guoqing, 2021. Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin. Earth Science, 46(7): 2379-2390. doi: 10.3799/dqkx.2020.252

Jia Xiaoyu, Gao Fuhong, Xiu Ming, Liu Guoqing, 2021. Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin. Earth Science, 46(7): 2379-2390. doi: 10.3799/dqkx.2020.252

Citation:

Jia Xiaoyu, Gao Fuhong, Xiu Ming, Liu Guoqing, 2021. Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin. Earth Science, 46(7): 2379-2390. doi: 10.3799/dqkx.2020.252

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Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin

doi: 10.3799/dqkx.2020.252

College of Earth Science, Jilin University, Changchun 130061, China

Received Date: 2020-08-21
Publish Date: 2021-07-15

Abstract

Abstract

To constrain the provenance characteristics and tectonic setting of the Late Cretaceous Furao and Taipinglinchang formations located in the Sunwu-Jiayin Bbasin, in this paper, the LA-ICP-MS U-Pb dating results of detrital zircons and the geochemical characteristics from the Furao and Taipinglinchang formations are studied.The 55 detrital zircons in Furao Formation yield age population of 65 Ma, 280 Ma and 496 Ma and 78 detrital zircons in Taipinglinchang Formation yield age populations of 98 Ma, 189 Ma, 240 Ma and 488 Ma, indicating that the Furao formation and Taipinglingchang Formation have the characteristics of mixture source.Al₂O₃/TiO₂ average value of the Furao and Taipinglinchang formations is 41.42 and 29.31, combined with major、trace and REE elements and detrital zircons yield age populations, determined that the provenance of the Furao and Taipinglinchang formations is mainly derived from the Late Mesozoic felsic igneous rocks and sedimentary rocks.The geochemical and regional tectonic evolution characteristics reveal that the tectonic setting of the provenance area of the Furao and Taipinglinchang formations is the active continental margin.The Late Mesozoic magmatic events, the Mashan Group in the northern part of Jiamusi Massif and the widely distributed Paleozoic granites provide sedimentary source for the Late Cretaceous strata of the basin.
- Sunwu-Jiayin basin,
- Furao Formation,
- Taipinglinchang Formation,
- U-Pb chronology,
- geochemistry,
- provenance,
- tectonic setting

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References(49)

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