1) Property of the Moho
莫霍界面性质
2) Moho
[英]['məuhəu] [美]['moho]
莫霍界面
1.
Airry isostatic anomalies and Moho-depth were calculated and analysed.
研究了该剖面及其邻区为主的青藏高原西北边缘重力场特征；划分了３个地质构造单元及８条较大断裂；计算并分析了Ａｉｒｙ重力均衡异常及莫霍界面深度。
2.
Subtracting the gravity anomalies caused by density anomalies from the observed Bouguer anomalies, we inversed the depth of Moho of northwestern China by using the residu- al anomalies.
在从观测布格重力异常中扣除上述密度异常引起的重力异常后的数据基础上,直接反演了中国西北区域莫霍界面的深度。
3) Moho boundary
莫霍面边界
4) Mohorovicic Discontinuity (Moho)
莫霍(洛维奇)不连续面;莫霍(洛维奇)界面
5) Moho
[英]['məuhəu] [美]['moho]
莫霍面
1.
Moho Depths Inversion of Qinghai-Tibet Plateau with Variable Density Model;
用变密度模型反演青藏高原的莫霍面深度
2.
The Study on the fluctuation of Moho in Yellow Sea and its adjacent area;
黄海及邻区莫霍面起伏特征
3.
It is confirmed that Jiyang depression of Paleogene occurred in trans-extensional behavior in the light of Moho uplifting,lithosphere thinning,development of basic and ultra basic igneous rocks in mantle source rocks,high geothermal gradient,halfgraben-like depression bas.
从8个方面(莫霍面上隆和岩石圈减薄、幔源基性火山岩和超基性岩的发育、高的地温梯度、一系列箕状断陷盆地群的伸展量高达50km以上及沉积速率高达0。
6) Moho discontinuity
莫霍面
1.
A Review on the Moho Discontinuity beneath the Tibetan Plateau;
青藏高原莫霍面的研究进展
2.
The infrastructure of this zone is apparently controlled by the transitional belt between the mantle slope of Yunyang backbone and the mantle flat of Xunyang on Moho discontinuity and by the western marginal rim of Wudang platform on Conrad discontinuity.
该矿带在深层构造上明显受莫霍面郧阳脊状幔坡与旬阳幔坪之间的过渡带和康拉德面武当坪台西部边缘的控制。
3.
Some new viewpoints were proposed concerning the trend and extension of the southwestern end of the Altun strike-slip fault,the origin of two low gravity zones was discussed,the altitude of the Moho discontinuity in the .
对阿尔金走滑断裂西南端的走向和延伸提出了一些新的看法;讨论了2条重力低值带的成因;推断了班公湖—怒江结合带下部莫霍面隆起的高度,从重力角度提出了对班公湖—怒江结合带的认识;认为青藏块体在拼合后地壳有2个加厚中心;新圈定了一个中、新生代沉积盆地,并进行了初步研究;结合地质、矿产、航磁等资料,初步划分出4个成矿远景区(带)。
补充资料：莫霍界面
莫霍界面 地壳和地幔的分界面。1909年A.莫霍洛维奇根据对克罗地亚的地震图的分析，识别出这一界面的存在，根据发现者的名字命名。又称莫霍洛维奇间断面。见地球内部构造。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条