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Short-term temporal variability of GPS receiver's differential code biases (DCB): retrieving and modeling GPS接收机差分码偏差(DCB)的短期时间变异性:检索与建模
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.6038/CJG20160109
Baocheng Zhang, Y. Yuan, J. Ou
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引用次数: 7
3D finite element modeling of marine controlled-source electromagnetic fields using locally refined unstructured meshes 海洋可控源电磁场的局部精细非结构化网格三维有限元建模
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.6038/CJG20161233
Yixin Ye, Li Yuguo, Y. Liu, Gang Li, Haiyan Yang
We present a 3D forward modeling algorithm of marine controlled-source electromagnetic (CSEM) fields using finite element method based on unstructured meshes. As the unstructured mesh is incorporated, the algorithm can easily accommodate complex structures, such as dipping interfaces and rough topography. Secondary coupled-potential formulation of Maxwell's equations allows to avoid the singularities introduced by the sources. The primary electromagnetic fields excited by electric dipole source in layered isotropic media are derived from the semi-analytical formulas based on Schelkunoff potentials. To improve the accuracy and efficiency of the algorithm, we propose an effective local mesh refinement strategy, where the elements near the receiver locations and in the abnormal areas are refined using the volume constraints. We validate the finite element code against a 1D and 2D reservoir model and study the performance of the local mesh refinement strategy. The Canonical disc model illustrates the utility of the finite element method for 3D CSEM modeling. The bathymetry model study shows that the seafloor topography gives an important response which needs to be reproduced by numerical modeling to avoid the misinterpretation of measurements.
提出了一种基于非结构化网格的海洋可控源电磁场三维正演建模算法。由于加入了非结构化网格,该算法可以方便地适应倾斜界面和粗糙地形等复杂结构。麦克斯韦方程组的二次耦合势公式可以避免源引入的奇点。利用基于舍尔库诺夫势的半解析公式,推导了层状各向同性介质中电偶极子源激发的一次电磁场。为了提高算法的精度和效率,我们提出了一种有效的局部网格细化策略,利用体积约束对靠近接收器位置和异常区域的单元进行细化。我们针对一维和二维油藏模型验证了有限元代码,并研究了局部网格细化策略的性能。典型圆盘模型说明了有限元法在三维CSEM建模中的实用性。测深模型研究表明,海底地形是一个重要的响应,需要通过数值模拟来再现,以避免测量结果的误读。
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引用次数: 2
Cenozoic mountain-building processes in the Daliangshan, southeastern margin of the Tibetan Plateau: Evidence from low-temperature thermochronology and thermal modeling 青藏高原东南缘大凉山新生代造山过程:来自低温年代学和热模拟的证据
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.15496/PUBLIKATION-14471
B. Deng
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引用次数: 8
GNSS radio occultation technique for near-Earth space environment detection 近地空间环境探测GNSS无线电掩星技术
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.6038/cjg20160401
X. Yue, Yongxin Guo, Z. Zeng, W. Wan
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引用次数: 4
Source parameters for the 2015 Nepal earthquake revealed by InSAR observations and strong ground motion simulation 2015年尼泊尔地震InSAR观测和强地震动模拟的震源参数
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.6038/CJG20160417
Y. Li, W. Shen, Y. Wen, J. Zhang, Zhenhong Li, W. Jiang, Y. Luo
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引用次数: 7
The research of ocean tide loading effects on gravity and ambient noise at Zhongshan and Syowa station in Antarctic 南极中山站和洼地站潮汐载荷对重力和环境噪声的影响研究
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2016-01-01 DOI: 10.6038/cjg20160805
Liu Qing-chao, Sun He-ping, Xu Jianqiao, Lt, strong gt, Chen Xiao-Dong lt, Zhang Miao-miao, He Qian-qian
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引用次数: 0
Temporal-spatial variations of sea level over China seas derived from altimeter data of TOPEX/Poseidon, Jason-1 and Jason-2 from 1993 to 2012 基于TOPEX/Poseidon、Jason-1和Jason-2高度计资料的1993 - 2012年中国海域海平面时空变化
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2015-09-01 DOI: 10.6038/CJG20150908
Guo Jin-yun, Wang Jianbo, Hu Zhi-bo, C. Hwang, Chen Chuanfa, Gao Yong-gang
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引用次数: 30
Sedimentary evolution since Quaternary in the Shenhu hydrate drilling area, northern South China Sea 南海北部神狐水合物钻探区第四纪以来沉积演化
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2015-08-01 DOI: 10.6038/CJG20150829
Su Ming, Sha Zhi-bin, Qi Shao-hua, Y. Rui, Wu Nengyou, Cong Xiaorong, L. Jie
The marine gas hydrate samples in China were for the first time acquired in the Shenhu area,northern continental slope of the South China Sea.However,due to erosion by the submarine canyons,the stratigraphic comparison and identification of sedimentary facies were difficult,leading to the lack of description of seismic-sedimentary facies,analysis of forming mechanisms and distribution of the sedimentary units.Moreover,few researches focused on the sedimentary evolution since Quaternary,and the crucial controlling factors on the heterogeneous distribution of gas hydrate are not clearly understood.Using high-resolution 2D/3Dseismic data,this study attempts to classify the seismic facies and discuss the sedimentary evolution in this area since Quaternary.This work is based on the high-resolution 2Dand 3Dseismic data obtained by Guangzhou Marine Geological Survey in 2006,with a trace interval of 12.5mand vertical resolution of 10~20 m.Firstly,we make an integrated analysis of seafloor topographic features,sequence stratigraphic framework and high-resolution seismic data,perform a classification of seismic facies have been classified,and describe morphological features and internal architectures accurately.Secondly,in terms of sediment supplies from the north and seafloor topography,deep-water sedimentary process is analyzed.Also,the sedimentary evolutions since Quaternary are re-built.Subsequently,the relationship between deep-water sediments since Quaternary and distribution of gas hydrates are discussed.Five types of seismic facies were identified,involving prograding slopes,small-scale turbidite channels in the Early Quaternary,sediment failures(including slides and slumps),submarine canyons and concomitant transformation of deposits,and the mixture of abysmal deposits and mass transport complex.The three phases of sedimentary evolution since Quaternary in the Shenhu area were re-built,which are turbidite channels erosion and re-deposited sediments,prograding slopes and sediments failures,and erosion and sedimentation of submarine canyons.Eroded by small-scale turbidites,re-deposited sediments would be near-source stacked with relatively good property conditions,which might be regarded as the potential suitable reservoirs for gas hydrates.The deposits transported from prograding slopes could lose the balance easily and result in sediments failures widespread in the Shenhu area.Because of the fine-grain particle and vertical continuity,sediment failures could be thought as the regional cap rock.Abundant submarine canyons and concomitant transformation of deposits could erode and destroy underlying strata,which modified suitable deposits as patch distribution.Hence,the sedimentary evolution since Quaternary was considered as one of the crucial controlling factors on the heterogeneous distribution of gas hydrate in the Shenhu hydrate drilling area,northern South China Sea.
中国首次在南海北部陆坡神狐海域获得海相天然气水合物样品。然而,由于海底峡谷的侵蚀作用,沉积相的地层比较和识别困难,导致地震-沉积相的描述、沉积单元的形成机制和分布分析缺乏。此外,第四纪以来的沉积演化研究较少,对天然气水合物非均质分布的关键控制因素认识不清。利用高分辨率二维/三维地震资料,对该区第四纪以来的地震相进行分类,探讨该区的沉积演化。本文基于广州海洋地质调查局2006年获得的二维和三维高分辨率地震资料,道距为12.5,垂向分辨率为10~20 m。首先,综合分析海底地形特征、层序地层格架和高分辨率地震资料,对已分类的地震相进行分类,准确描述形态特征和内部构型;其次,从北方输沙和海底地形出发,分析了深水沉积过程。重建了第四纪以来的沉积演化过程。讨论了第四纪以来深水沉积与天然气水合物分布的关系。确定了5种地震相类型,分别为:前冲积坡相、早第四纪小尺度浊积河道相、沉积失稳(包括滑坡和滑塌)相、海底峡谷相和沉积伴生转化相、深海沉积与块体搬运杂岩相混合相。重建神狐地区第四纪以来的沉积演化3个阶段,即浊积岩河道侵蚀与再沉积、进坡与沉积物破坏、海底峡谷侵蚀与沉积。再沉积沉积物受小尺度浊积岩侵蚀,形成近源堆积,物性条件较好,可视为天然气水合物的潜在适宜储层。从进坡搬运的沉积物容易失去平衡,导致沈狐地区普遍存在沉积物失稳现象。由于其颗粒细、纵向连续性强,可将其视为区域性盖层。丰富的海底峡谷及其伴生的矿床改造对下伏地层具有侵蚀和破坏作用,使适宜矿床呈斑块状分布。因此,第四纪以来的沉积演化被认为是南海北部神狐水合物钻探区天然气水合物非均质分布的重要控制因素之一。
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引用次数: 11
Applications and challenges of near surface geophysics in geotechnical engineering 近地表地球物理在岩土工程中的应用与挑战
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2015-08-01 DOI: 10.6038/CJG20150806
Chih‐Ping Lin, Chun-Hung Lin, Po-Lin Wu, Hsin-Chang Liu, Ying-Chun Hung
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引用次数: 11
Trends of glacial mass changes in High Asia from satellite gravity observations 从卫星重力观测看高亚洲冰川质量变化趋势
IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2015-03-01 DOI: 10.6038/CJG20150309
Chuandong Zhu, Yang Lu, Hongling Shi, Zizhan Zhang, Z. Du, Chunchun Gao
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引用次数: 0
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