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摘要:
An intensive magnetic anomaly within the limits of West Siberia Danilov graben-rift indicates magnetic rocks while numerous wells encountered only weakly magnetized Triassic basalts and liparites in the basement covered by thick loose Jurassic and younger sediments. The wells penetrated only the first tens meters of the basement and could not tell us about the liparites structure at depth where supposedly they may form a big single body and magnetic rocks may be situated deeper. Geological ideas on a graben-rift structure may be proved (or rejected) by a computer modeling of its magnetic properties. For the anomalous geomagnetic field interpretation, a method of volume integral equations taking into account demagnetization effect was employed. To fit a model a trial-and-error procedure was utilized. The results show that 1) at the depth some rocks are magnetized in opposite direction to the present field;2) highly magnetized rocks (magnetic susceptibility 0.06 - 0.1SI) coming up continuously from the bottom of the model and situated under the graben;3) the studied structure is not a graben but the rift because the continental light crust is absent.
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篇名 Anomalous Geomagnetic Field Modeling for Crustal Structure of a Graben in West Siberia
来源期刊 地质学期刊(英文) 学科 医学
关键词 Graben-Rift GEOMAGNETIC ANOMALY Modeling INTEGRAL Equation Interpretation
年,卷(期) 2018,(3) 所属期刊栏目
研究方向 页码范围 232-246
页数 15页 分类号 R73
字数 语种
DOI
五维指标
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研究主题发展历程
节点文献
Graben-Rift
GEOMAGNETIC
ANOMALY
Modeling
INTEGRAL
Equation
Interpretation
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研究去脉
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期刊影响力
地质学期刊(英文)
月刊
2161-7570
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
585
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0
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0
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