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摘要:
The existence of mafic bodies at mid crustal level beneath the Pan-African Central Cameroon Shear Zone is still a matter of debate. To provide additional constrains on this issue, the crust of the west region of Cameroon has been investigated using gravity data. Analyses of these data show N40-50°E oriented iso-anomal contours in the Bafoussam area, interpreted as the N40-50°E branch of the Central Cameroon Shear Zone. In addition, spectral analysis and 2.5D gravity modeling reveal intrusions of mafic bodies at depth between 3.2 and 14.2 km under N40-50°E aligned volcanic centers, namely Mt Bambouto and Mt Mbapit. The above observations suggest a structurally controlled emplacement of the mafic bodies. In the light of the recent geophysical data, the interaction between the NE-ward channel flow operating at the bottom of the lithosphere or the asthenosphere upwelling and the Cameroon Shear Zone could better explain the magma upwelling in the upper crust. This result is the novelty of the present work.
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篇名 Evidence for the Upwelling of Mafic Bodies into the Upper Crust beneath the N40-50°E Branch of the Pan-African Central Cameroon Shear Zone from Gravity Studies
来源期刊 地质学期刊(英文) 学科 地球科学
关键词 West Region MAFIC BODIES CENTRAL Cameroon Shear Zone GRAVITY 2.5D Modelling
年,卷(期) 2018,(3) 所属期刊栏目
研究方向 页码范围 278-297
页数 20页 分类号 P5
字数 语种
DOI
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节点文献
West
Region
MAFIC
BODIES
CENTRAL
Cameroon
Shear
Zone
GRAVITY
2.5D
Modelling
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
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
总下载数(次)
0
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0
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