舒兰—尚志断裂带地质及地球物理场特征
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摘要
舒兰—尚志断裂是依兰—伊通断裂的中段,通过布格重力异常和航磁△T异常的分析及数据处理、场的转换、异常分离、重力、航磁、地震综合解释确定F1、F2、F3、F4、F5为主要断裂。通过地质特征对该区地层、岩浆活动有一定了解。对断裂盆地认识及从区域性了解第三纪含煤建造特征与构造体系的关系。通过资料总结为后期煤炭资源勘查提出建议和方案。
The zone of Sulan-Shangzhi fault is the middle part of Yilan-Yitong fracture,through the analysis of the Bouguer gravity and aeromagnetic △T anomaly and data processing,the conversion of field,anomaly separation,the synthetical explanation of gravity,aeromagnetic and earthquake,the authors determined F1,F2,F3,F4,F5 are the main faults.Through Geological features,the authors understood the stratum and magmatic activities in the area.The understanding of fault basin and the relationship between the Tertiary coal-bearing characteristics of the construction and the tectonic system from the region.Through the information summary,it put forward programmes and proposals for the exploration of coal resources later.
引文
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    [4]穆克敏,申宁华,孙运生.区域地球物理数据方法及其应用[M].长春:吉林科学技术出版社,1990.
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    [6]张作新等.吉林省敦化地区重磁普查勘探成果报告[R].1998.

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