Provenance and Tectonic Setting of the Late Cretaceous Strata in Sunwu-Jiayin Basin
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摘要: 为揭示孙吴-嘉荫盆地晚白垩世富饶组和太平林场组的物源特征及其构造背景，对两组样品进行了碎屑锆石LA-ICP-MS U-Pb定年和地球化学特征研究.富饶组碎屑锆石55个测点产生以下年龄峰值：65 Ma、280 Ma和496 Ma，太平林场组碎屑锆石78个测点产生以下年龄峰值：98 Ma，189 Ma，240 Ma和488 Ma，表明富饶组和太平林场组具有混合物源的特征.Al2O3/TiO2平均值分别为41.42和29.31，结合主量、微量及稀土元素特征和碎屑锆石峰值年龄，确定富饶组和太平林场组物源主要为晚中生代长英质火成岩和沉积岩.地球化学和区域构造演化特征共同揭示富饶组和太平林场组物源区构造背景为活动大陆边缘，区域内晚中生代岩浆事件、佳木斯地块北部麻山群及广泛分布的古生代花岗岩为盆地晚白垩世地层提供了沉积物源.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.
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Key words:
- Sunwu-Jiayin basin /
- Furao Formation /
- Taipinglinchang Formation /
- U-Pb chronology /
- geochemistry /
- provenance /
- tectonic setting
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图 2 富饶组和太平林场岩性柱状图及采样位置
Fig. 2. Column diagrams of the Furao and Taipinglinchang formations showing lithology and sampling locations
图 3 富饶组和太平林场组野外露头和样品显微照片
Fig. 3. Outcrop photographs and photomicrographs of samples from the Furao and Taipinglinchang formations
图 4 样品JY-4-1代表性锆石阴极发光图像
Fig. 4. CL images of the representative zircons from the sample JY-4-1
图 5 样品JY-4-1锆石LA-ICP-MS U-Pb谐和图
Fig. 5. Zircon LA-ICP-MS U-Pb concordia diagrams for the sample JY-4-1
图 6 样品JY-6-1代表性锆石阴极发光图像
Fig. 6. CL images of the representative zircons from the sample JY-6-1
图 7 样品JY-6-1锆石LA-ICP-MS U-Pb谐和图
Fig. 7. Zircon LA-ICP-MS U-Pb concordia diagrams for the sample JY-6-1
图 8 富饶组和太平林场组风化特征
Fig. 8. Diagrams of weathering characteristics for the Furao and Taipinglinchang formations
图 9 富饶组和太平林场组样品稀土元素球粒陨石标准化曲线
Fig. 9. Chondrite-normalized REE patterns of samples from the Furao and Taipinglinchang formations
图 10 富饶组和太平林场组样品稀土元素PAAS标准化曲线
Fig. 10. PAAS-normalized REE patterns of samples from the Furao and Taipinglinchang formations
图 11 富饶组和太平林场组源岩类型判别图解
Fig. 11. Discrimination diagrams of source rock types of the Furao and Taipinglinchang formations
图 12 富饶组碎屑锆石U-Pb年龄分布直方图
Fig. 12. U-Pb age distribution histogram of detrital zircons from the Furao Formation
图 13 太平林场组碎屑锆石U-Pb年龄分布直方图
Fig. 13. U-Pb age distribution histogram of detrital zircons from the Taipinglinchang Formation
图 14 富饶组和太平林场组沉积岩构造背景判别图解
A.大洋岛弧；B.大陆岛弧；C.活动大陆边缘；D.被动大陆边缘
Fig. 14. Tectonic setting discriminate diagrams of sedimentary rocks of the Furao and Taipinglinchang Formations
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