Journal of Tropical Oceanography ›› 2022, Vol. 41 ›› Issue (5): 43-56.doi: 10.11978/2021162CSTR: 32234.14.2021162
Special Issue: 海洋大数据及应用
• Marine Geophysics • Previous Articles Next Articles
GUO Jian1,2,3,4(), QIU Xuelin1,2,3,4(), LI Zizheng1,2,3,4, HUANG Haibo1,2,3
Received:
2021-11-22
Revised:
2022-01-18
Online:
2022-09-10
Published:
2022-01-19
Contact:
QIU Xuelin
E-mail:guojian@scsio.ac.cn;xlqiu@scsio.ac.cn
Supported by:
CLC Number:
GUO Jian, QIU Xuelin, LI Zizheng, HUANG Haibo. Data processing and phase identification of OBS2019-2 in Nansha Block*[J].Journal of Tropical Oceanography, 2022, 41(5): 43-56.
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Tab. 1
OBS relocation results of OBS2019-2"
站位 编号 | OBS 编号 | 投放点位置 | 校正后位置 | 校正后 水深/m | RMS/ms | t_adjust/s | ||
---|---|---|---|---|---|---|---|---|
经度/E | 纬度/N | 经度/E | 纬度/N | |||||
01 | A37 | 115°05′35.48″ | 12°49′05.95″ | 115°05′40.02″ | 12°49′06.31″ | 4360 | 2.6 | -3.033 |
02 | L26 | 115°07′43.72″ | 12°44′24.97″ | 115°07′51.46″ | 12°44′28.46″ | 4361 | 1.3 | -0.144 |
03 | S11 | 115°09′51.84″ | 12°39′43.92″ | 115°09′46.73″ | 12°39′40.97″ | 4363 | 1.8 | -0.117 |
04 | L23 | 115°12′00.40″ | 12°35′03.62″ | 115°11′48.66″ | 12°34′58.58″ | 4358 | 3.4 | -0.124 |
05 | L85 | 115°14′07.84″ | 12°30′21.82″ | 115°14′09.71″ | 12°30′20.84″ | 4360 | 1.2 | -1.157 |
06 | B41 | 115°16′15.74″ | 12°25′40.76″ | 115°16′11.39″ | 12°25′40.58″ | 4357 | 1.4 | -0.011 |
07 | L54 | 115°18′23.54″ | 12°20′59.68″ | 115°18′19.80″ | 12°20′59.53″ | 4359 | 1.5 | -0.144 |
08 | L16 | 115°20′31.31″ | 12°16′18.55″ | 115°20′44.09″ | 12°16′24.71″ | 4357 | 1.9 | -0.126 |
09 | H56 | 115°22′38.96″ | 12°11′37.43″ | 115°22′24.17″ | 12°11′32.75″ | 4357 | 1.5 | -0.108 |
10 | L17 | 115°24′46.55″ | 12°06′56.30″ | 115°24′48.20″ | 12°07′00.08″ | 4359 | 1.9 | -0.130 |
11 | B29 | 115°26′54.06″ | 12°02′15.14″ | 115°26′31.38″ | 12°02′07.55″ | 4369 | 3.1 | -2.928 |
12 | L94 | 115°29′01.50″ | 11°57′33.95″ | 115°28′58.40″ | 11°57′33.95″ | 4326 | 0.7 | -1.115 |
13 | L96 | 115°31′08.87″ | 11°52′52.75″ | 115°31′09.48″ | 11°52′54.84″ | 4328 | 2.2 | -0.111 |
14 | L93 | 115°33′16.16″ | 11°48′11.56″ | 115°33′22.93″ | 11°48′14.18″ | 4321 | 1.7 | -0.122 |
15 | L35 | 115°35′23.39″ | 11°43′30.32″ | 115°35′12.37″ | 11°43′25.46″ | 4332 | 2.0 | -0.028 |
17 | B87 | 115°39′37.62″ | 11°34′07.86″ | 115°39′22.03″ | 11°34′00.05″ | 4070 | 2.3 | -0.027 |
18 | L70 | 115°41′45.31″ | 11°29′27.67″ | 115°41′31.38″ | 11°29′21.12″ | 3936 | 1.4 | -0.115 |
19 | L98 | 115°43′51.56″ | 11°24′45.29″ | 115°44′03.70″ | 11°24′49.57″ | 3104 | 3.3 | -0.076 |
20 | L95 | 115°45′58.43″ | 11°20′03.98″ | 115°45′38.92″ | 11°19′55.81″ | 2700 | 1.8 | -0.093 |
23 | B40 | 115°52′18.59″ | 11°05′60.00″ | 115°52′18.84″ | 11°06′00.07″ | 2142 | 4.2 | 0.039 |
24 | L31 | 115°54′25.20″ | 11°01′18.66″ | 115°53′52.12″ | 11°01′04.76″ | 2675 | 5.2 | -2.093 |
25 | L64 | 115°56′31.70″ | 10°56′37.28″ | 115°56′36.89″ | 10°56′40.06″ | 2350 | 5.5 | -0.099 |
27 | D28 | 116°00′44.57″ | 10°47′14.50″ | 116°00′43.31″ | 10°47′14.32″ | 2114 | 3.1 | -0.192 |
28 | L89 | 116°02′50.89″ | 12°49′05.95″ | 116°02′50.82″ | 10°42′33.16″ | 2228 | 3.5 | -1.893 |
29 | H52 | 116°04′57.14″ | 12°44′24.97″ | 116°04′43.25″ | 10°37′45.48″ | 2103 | 2.1 | 0.068 |
30 | L99 | 116°07′03.07″ | 12°39′43.92″ | 116°07′02.82″ | 10°33′09.86″ | 1794 | 3.9 | 0.054 |
Fig. 6
Seismic phase identification and the travel-time ray tracing in the vertical component of seismic record of OBS11. (a) The seismic record profile and the seismic phase identification (the reduced velocity is 6.0 km·s-1); (b) Travel-time fitting (the black thin lines show the calculated travel-times and the thick colored lines show the picked travel-times); (c) The initial model of P-wave and ray-tracing of the seismic phases"
Fig. 7
Vertical component of the seismic record in OBS14 and the seismic phase identification. (a) The seismic record profile and the seismic phase identification (the reduced velocity is 6.0 km·s-1); (b) Travel-time fitting (the black thin lines show the calculated travel-times and the thick colored lines show the picked travel-times); (c) The initial model of P-wave and ray-tracing of the seismic phases"
Fig. 8
Vertical component of the seismic record in OBS17 and the seismic phase identification. (a) The seismic record profile and the seismic phase identification (the reduced velocity is 6.0 km·s-1); (b) Travel-time fitting (the black thin lines show the calculated travel-times and the thick colored lines show the picked travel-times); (c) The initial model of P-wave and ray-tracing of the seismic phases"
Fig. 9
Vertical component of the seismic record in OBS23 and the seismic phase identification. (a) The seismic record profile and the seismic phase identification (the reduced velocity is 6.0 km·s-1); (b) Travel-time fitting (the black thin lines show the calculated travel-times and the thick colored lines show the picked travel-times); (c) The initial model of P-wave and ray-tracing of the seismic phases"
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