最近20年来建立起来的一门新兴的边缘学科。它利用古地磁学和岩石磁学的技术与方法,测定在不同环境条件下岩石磁性各种参数所发生的变化,去研究岩石磁性与环境变化的关系,进而研究环境演变的规律
This thesis depends on geochemistry and environmental magnetism to reveal environmental evolution of Honghu Lake.
本文以地球化学和环境磁学作为环境代用指标,通过对它们的解译来研究洪湖的环境演化。
参考来源 - 洪湖近1300年来的环境演变研究·2,447,543篇论文数据,部分数据来源于NoteExpress
对尘土、不同深度的表土和沙尘暴样品开展了系统的环境磁学参数测量。
Environmental Magnetic measurements were carried out on all urban dust, topsoil and dust storm samples.
对西苕溪流域的土壤样品及部分太湖近岸表层底泥样品,进行了环境磁学测试与化学分析。
Soil samples in the Tiaoxi Catchment, mostly in West Tiaoxi Catchment, as well as some sediments in Taihu Lake, were collected and analyzed with magnetic properties and heavy metal concentrations.
为了识别古洪灾事件,因而从环境磁学角度建立两种沉积物的识别标志是非常必要和有意义的。
In order to identify the ancient flood disaster events, it is significant to establish identification marks of sediments from the environment magnetism.
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