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목차보기

목차

표제지=0,1,1

제출문=1,2,2

요약문=3,4,4

SUMMARY=7,8,1

List of Figures=8,9,4

List of Tables=11,12,2

목차=13,14,2

제1장 서론=15,16,3

제2장 국내외 기술개발 현황=18,19,2

제3장 연구개발수행 내용 및 결과[내용누락;p.28]=20,21,77

제4장 연구개발목표 달성도 및 결과의 활용계획=97,98,1

참고 문헌=98,99,5

부록=103,104,80

그림목차

Fig. 3-1-1. Geophysical survey tracks for 2002 marine geological mapping project. The open circles denote the CMP positions acquired during multi-channel digital seismic survey. The crossed dots denote piston core sites to evaluate surface and shallow sub=16,17,1

Fig. 3-1-1-1. A flow chart showing the data acquisition and reprocessing using Trinav navigation system=21,22,1

Fig. 3-1-1-2. The offset diagram of the several shipborne and 2D reflection seismic equipment used in this survey=25,26,1

Fig. 3-1-4-1. The diagram of magnetic survey=30,31,1

Fig. 3-2-1-1. Multichannel profile showing the sequences I,II,III and IV. The sequence IV has subparallel reflection configuration and hummocky seismic facies. The sequences I and III have subparallel reflection configuration and sequence II has weak...=33,34,1

Fig. 3-2-1-2. Isopac map of total sediments. Contour interval is 0.1 seconds in two way travel time=35,36,1

Fig. 3-2-1-3. Multichannel profile showing the sedimentary acoustic basement=36,37,1

Fig. 3-2-1-4. Multichannel profile showing the volcanic acoustic basement=37,38,1

Fig. 3-2-1-5. Isopac map of sequence IV. Contour interval is 0.1 seconds in two way travel time=38,39,1

Fig. 3-2-1-6. Multichannel profile showing the sequences I,II,and IV. The sequence IV has steep subparallel reflection configuration and hummocky seismic facies. The sequence II has weak and uncontinuous subparallel reflection configuration and chaotic...=40,41,1

Fig. 3-2-1-7. Multichannel profile showing the sequences I,II,III and IV. The sequence IV has subparallel reflection configuration and hummocky seismic facies. The sequences I and III have subparallel reflection configuration and sequence II has weak...=42,43,1

Fig. 3-2-1-8. Isopac map of sequence III. Contour interval is 0.1 seconds in two way travel time=43,44,1

Fig. 3-2-1-9. Isopac map of sequence II. Contour interval is 0.05 seconds in two way travel time=44,45,1

Fig. 3-2-1-10. Isopac map of sequence I. Contour interval is 0.05 seconds in two way travel time=46,47,1

Fig. 3-2-2-1. The height difference between known absolute value of Jangchon and gravity meter of Tamhae II=49,50,1

Fig. 3-2-2-2. Free-air gravity anomaly map for 2002 survey=53,54,1

Fig. 3-2-3-1. Total intensity anomaly map for 2002 survey=55,56,1

Fig. 3-2-4-1 Bathymetric map of the study area based on single beam echosounder. The contour interval is 5m. Note the submarine topographic low running from north to south. It is also noteworthy of ridge-shaped topographic high In the eastern central...=57,58,1

Fig. 3-2-5-1. High-resolution (3.5 kHz) seismic profile collected from the southwestern part of the study area showing four sedimentary units above the acoustic basement=60,61,1

Fig. 3-2-5-2. High-resolution (3.5 kHz) seismic profile collected from the southern part of the study area showing two sedimentary units=60,61,1

Fig. 3-2-5-3. High-resolution (3.5 kHz) seismic profile collected from the southwestern part of the study area showing three sedimentary units=61,62,1

Fig. 3-2-5-4. High-resolution (3.3 kHz) seismic profile collected from the southeastern part of the study area showing Unit II units directly overlying the acoustic basement=61,62,1

Fig. 3-2-5-5. High-resolution (3.5 kHz) seismic profile collected from the northern part of the study area showing Unit II directly overlying acoustic basement=62,63,1

Fig. 3-2-5-6. High-resolution (3.5 kHz) seismic profile collected from the northeastern part of the study area showing Unit II=62,63,1

Fig. 3-2-6-1a. Columnar description of piston core P01=72,73,1

Fig. 3-2-6-1b. Columnar description of piston core P07=73,74,1

Fig. 3-2-6-2a. Columnar description of piston core P04=74,75,1

Fig. 3-2-6-2b. Columnar description of piston core P05=75,76,1

Fig. 3-2-6-2c. Columnar description of piston core P09=76,77,1

Fig. 3-2-6-2d. Columnar description of piston core P10=77,78,1

Fig. 3-2-6-3a. Columnar description of piston core P11=78,79,1

Fig. 3-2-6-3b. Columnar description of piston core P12=79,80,1

Fig. 3-2-6-3c. Columnar description of piston core P14=80,81,1

Fig. 3-2-5-4a. Columnar description of piston core P17=81,82,1

Fig. 3-2-5-4b. Columnar description of piston core P18=82,83,1

Fig. 3-2-6-4c. Columnar description of piston core P22=83,84,1

Fig. 3-2-6-4d. Columnar description of piston core P25=84,85,1

Fig. 3-2-6-5a. Columnar description of piston core P19=85,86,1

Fig. 3-2-6-5b. Columnar description of piston core P20=86,87,1

Fig. 3-2-6-6a. Columnar description of piston core P26=87,88,1

Fig. 3-2-6-6b. Columnar description of piston core P27=88,89,1

Fig. 3-2-6-6c. Columnar description of piston core P29=89,90,1

Fig. 3-2-6-6d. Columnar description of piston core P31=90,91,1

Fig. 3-2-6-6e. Columnar description of piston core P32=91,92,1

Fig. 3-2-6-7. Distribution of surface sediment types based on the Folk's (1968) classification scheme. The study area is dominated by sand in northeastern part and mud in southwestern part with transitional sediment types (zS and sZ) in between.=93,94,1

Fig. 3-2-6-8. Distribution of mean grain size of surface sediments based on the Folk and Ward (1957) method. Note that the mean values are minimum(coarsest) in the middle following the topographic low. In the eastern central part of the study area...=94,95,1

표목차

Table 1. Seismic acquisition work order for 2001 survey[내용누락;p.28]=28,29,1

Table 2. Location of piston core samples=31,32,1

Table 3. Determination of absolute gravity value of Jangchon port=48,49,1

칼라목차

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Fig. 3-2-1-3. Multichannel profile showing the sedimentary acoustic basement=36,37,1

Fig. 3-2-1-4. Multichannel profile snowing the volcanic acoustic basement=37,38,1

Fig. 3-2-1-4. Multichannel profile showing the volcanic acoustic basement=40,41,1

Fig. 3-2-1-7. Multichannel profile showing the sequences I,II,III and IV. The sequence IV has subparallel reflection configuration and hummocky seismic facies. The sequences I and III have subparallel reflection configuration and sequence II has weak...=42,43,1

Fig. 3-2-2-2. Free-air gravity anomaly map for 2002 survey=53,54,1

Fig. 3-2-3-1. Total intensity anomaly map for 2002 survey=55,56,1

Fig. 3-2-6-7. Distribution of surface sediment types based on the Folk's (1968) classification scheme. The study area is dominated by sand in northeastern part and mud in southwestern part with transitional sediment types (zS and sZ) in between.=93,94,1

Fig. 3-2-6-8. Distribution of mean grain size of surface sediments based on the Folk and Ward (1957) method. Note that the mean values are minimum(coarsest) in the middle following the topographic low. In the eastern central part of the study area...=94,95,1

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