论文部分内容阅读
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7<
关于用电检查反窃电工作的思考
【摘 要】
：
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7
【出 处】
：
黑龙江科技学院学报
【发表日期】
：
2018年9期
其他文献
Evolution of the Late Cenozoic Tectonic Stress Regime in the Tianshui Basin, Northeast Tibetan Plate
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7
读了《扁鹊见蔡恒公》一文,人们总是喜欢嘲笑“讳疾忌医”的蔡恒公,把他当作“听不得批评,容不得异议”的反面典型。其实,如果我们静下心来对这则故事细加咀嚼,或许会有这样
Discovery of the Early Devonian Sinistral Shear in the Jiangshan-Shaoxing Fault Zone and its Tectoni
The Jiangshan–Shaoxing fault zone(JSFZ)was formed by the amalgamation of the Yangtze and Cathaysia blocks in the Neoproterozoic.Since the Paleozoic,the JSFZ ha
Petrogenesis of Early and Late Carboniferous Volcanic Rocks in the Yining Block: Constraints from Sr
The Yining Block is located in the southwestern part of the Central Asian Orogenic Belt(CAOB),which is characterized by widespread Carboniferous volcanic rocks.