Reply to Comment on ‘‘Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component’’ by Beiki and Pedersen

B. Oruç

首页> 外文期刊>Pure and Applied Geophysics >Reply to Comment on ‘‘Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component’’ by Beiki and Pedersen

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Reply to Comment on ‘‘Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component’’ by Beiki and Pedersen

机译：回复评论，作者：Beiki和Pedersen对“重力梯度张量不变量和垂直分量的简单致病源的深度估计”

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《Pure and Applied Geophysics》 |2012年第2期|p.279-280|共2页
作者
B. Oruç;
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Engineering Faculty, Department of Geophysical Engineering, Kocaeli University, Umuttepe Campus, 41380, İzmit/Kocaeli, Turkey;

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1. Reply to Comment on ""Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component" by Beiki and Pedersen [J] . Oru? B. Pure and Applied Geophysics . 2012,第1a2期

机译：对Beiki和Pedersen的““通过重力梯度张量不变式和垂直分量的简单原因源的深度估计””的评论答复
2. Comment on “Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component” by B. Oruç in Pure Appl. Geophys. 167 (2010), 1259–1272 [J] . Majid Beiki, Laust B. Pedersen Pure and Applied Geophysics . 2012,第1a2期

机译：B.Oruç在Pure Appl中的评论“根据重力梯度张量不变式和垂直分量对简单原因的深度估计”。地理学。 167（2010），1259–1272
3. Comment on "Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component" by B. Oru? in Pure Appl. Geophys. 167 (2010), 1259-1272 [J] . Beiki Majid, Pedersen Laust Pure and Applied Geophysics . 2012,第1a2期

机译：评论B. Oru撰写的“根据重力梯度张量不变式和垂直分量对简单原因的深度估计”？在Pure Appl中。地理学。 167（2010），1259-1272
4. FULL GRAVITY GRADIENT TENSOR OF A VERTICAL PYRAMID MODEL OF FLAT TOP BOTTOM WITH DEPTH-WISE LINEAR DENSITY VARIATION [C] . Anand P. Gokula, Rambhatla G. Sastry Symposium on the Application of Geophysics to Engineering and Environmental Problems . 2016

机译：平顶＆底部垂直金字塔模型的全重力梯度张量，深度明智的线性密度变化
5. Joint Estimation of Source Range and Depth Using a Bottom-Deployed Vertical Line Array in Deep Water [O] . Hui Li, Kunde Yang, Rui Duan, 2017

机译：使用底部部署的垂直线阵列在深水中联合估算源范围和深度
6. Derived the complete gravity gradient tensor from the vertical component of gravity by a cosine transform technique [O] . Fuyu Jiang, Likun Gao 2010

机译：通过余弦变换技术从重力的垂直分量衍生完全重力梯度张量

Reply to Comment on ‘‘Depth Estimation of Simple Causative Sources from Gravity Gradient Tensor Invariants and Vertical Component’’ by Beiki and Pedersen

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