首页|江西彭山穹隆构造成因及地质意义

江西彭山穹隆构造成因及地质意义

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为探讨彭山穹隆成因及时代,在彭山地区开展了野外地质调查、构造解析和年代学等研究工作.结果表明,彭山穹隆为构造穹隆,形态为短轴背斜,其及周边存在稳定的印支期近SN向古构造应力场,伴生NNE向走滑断层,其东侧发育东倾的逆断层.切穿穹隆的断层被霏细斑岩脉贯入,霏细斑岩脉的锆石U-Pb年龄为(123.0±1.0)Ma,隐伏黑云母花岗岩的U-Pb年龄为(123.0±1.4)Ma,古应力场同期断层中断层泥的伊利石K-Ar年龄为(228.1±10.3)~(233.2±6.5)Ma,因此认为彭山穹隆形成时间为印支期或更早.
The Formation and Geological Significance of the Pengshan Dome in Jiangxi Province
To investigate the genesis and the age of the Pengshan dome,field geological surveys,structural analy-ses,and chronological studies were conducted in Pengshan area.The results show that the Pengshan dome is a tectonic dome with a short axis anticline in shape.There is a stable Indosinian-period paleotectonic stress field ori-ented nearly SN in and around the dome,associated with NNE-trending strike-slip faults,and an eastward-dipping thrust fault on its eastern side.Felsite porphyry dykes have intruded the faults which cut through the dome.The zircon U-Pb age of the felsite porphyry dykes is(123.0±1.0)Ma,the U-Pb age of the underlying rock mass is(123.0±1.4)Ma,and the illite K-Ar age of the fault gouge in the paleostress field is(228.1±10.3)~(233.2±6.5)Ma.Therefore,the formation time of the Pengshan dome is Indosinian or earlier.

domestructural geochronologyJiangnan orogenic beltPengshan

史洪峰、刘明军、孙强、朱延辉、张景

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中国地质调查局南京地质调查中心,江苏南京 210016

泰顺县自然资源和规划局,浙江温州 325500

穹隆 构造年代学 江南造山带 彭山

2024

东华理工大学学报(自然科学版)
东华理工学院

东华理工大学学报(自然科学版)

北大核心
影响因子:0.634
ISSN:1674-3504
年,卷(期):2024.47(4)