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제안 방법
- These cases, which frequently occur in marine geophysical data, should be eliminated to avoid improper XOPs. One of the easiest ways to resolve these problems is to do an additional straddle test with the opposite assignment for the initial line segment: C and D as the reference segment, and A and B as the comparing segment. The following equations determine the orientation of A relative to D with respect to C (Z3), and the orientation of B relative to D with respect to C (Z4):
- Since linked lists allocate the memory space dynamically, it only requires a small amount of memory size. This method was also applied to do a statistical analysis of data, and to provide the information of XOEs and weighting values.
- This study introduces a new and very simplemethod called a straddle test that uses a line intercepting algorithm and a linear equation to find all XOPs in any given dataset, and MittaFs algorithm (1984) was then adopted to correct and smooth the XOEs. Also, to effectively control computer memories and manage the data, a linked list algorithm was implemented instead of assigning a dimension of each I/O parameter.
- To examine the validity and efficiency of the developed algorithm and program, EZXover program was tested with the Free-Air gravity data obtained over a seamount in the East Sea, Korea. The data was collected by NORI (Korea National Oceanographic Research Institute) in 1997, and was composed of 9 track lines with 5 NS, 3 EW, and 1 NW-SE direction (Fig.
대상 데이터
- Korea. The data was collected by NORI (Korea National Oceanographic Research Institute) in 1997, and was composed of 9 track lines with 5 NS, 3 EW, and 1 NW-SE direction (Fig. 4). Line numbers 6 and 7, and 5 and 8 were surveyed on the same track, respectively.
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