Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (3): 96-115.doi: 10.11978/2022133CSTR: 32234.14.2022133
• Marine Geology • Previous Articles Next Articles
ZHAO Zhongxian1,2,3(), SUN Zhen1,3(
), MAO Yunhua4, ZHANG Huodai2
Received:
2022-06-10
Revised:
2022-08-15
Online:
2023-05-10
Published:
2022-09-07
Supported by:
ZHAO Zhongxian, SUN Zhen, MAO Yunhua, ZHANG Huodai. Heterogeneous extension and pulsed tectonic subsidence in the northern South China Sea margin*[J].Journal of Tropical Oceanography, 2023, 42(3): 96-115.
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Fig. 1
Regional structural map (a) and topography and data distribution of the South China Sea (b). The South China Sea Basin is composed of the eastern sub-basin, the northwestern sub-basin and the south-western sub-basin. The white short lines are the seafloor magnetic anomalies (Briais et al, 1993). In the northern continental margin of the South China Sea, there are the Yinggehai, Qiongdongnan, Pearl River Mouth and Taixinan Basins from west to east. The gray straight lines are multi-channel seismic survey lines, and the red dots mark the oil and gas wells and IODP drilling cites. The bold red lines 1-4 stand for four reflection seismic lines used here, and points P1-24 are selected to perform the detailed tectonic subsidence analysis."
Tab. 1
Fault growth rates along line 1"
断层 | 活动速率/(m·Myr-1) | ||||
---|---|---|---|---|---|
45—33.9Ma | 33.9—28.4Ma | 28.4—25.5Ma | 25.5—23Ma | 23—0Ma | |
F1 | 120.8 | 283.5 | 236.2 | 232.0 | - |
F4 | 9.8 | 16.2 | 58.0 | 29.6 | - |
F5 | 70.7 | 82.4 | 57.7 | 46.2 | - |
F6 | 125.9 | 85.5 | 201.2 | 26.7 | - |
F7 | 43.1 | 62.0 | 271.5 | - | - |
F8 | 35.9 | 83.6 | 88.7 | - | - |
F9 | 122.1 | 99.5 | 205.4 | - | - |
F10 | 178.3 | 339.8 | 370.4 | 200.5 | - |
F14 | - | 121.7 | 109.9 | 181.0 | - |
F15 | - | 60.4 | 26.4 | 55.1 | - |
F16 | - | - | - | 78.3 | - |
F17 | - | - | - | 54.9 | - |
F18 | - | 43.6 | 67.6 | 317.6 | - |
F19 | 31.5 | 55.5 | - | 231.5 | - |
F20 | 22.2 | 29.2 | - | 140.6 | - |
平均 | 71.1 | 90.0 | 145.7 | 123.8 | 0 |
Tab. 2
Fault growth rates along line 2"
断层 | 活动速率/(m·Myr-1) | ||||
---|---|---|---|---|---|
45—33.9Ma | 33.9—28.4Ma | 28.4—25.5Ma | 25.5—23Ma | 23—0Ma | |
F1 | - | 45.9 | 135.0 | 370.4 | - |
F2 | - | 74.3 | - | 41.9 | - |
F3 | 57.3 | 178.6 | - | - | - |
F4 | 116.4 | 20.3 | - | - | - |
F5 | 39.3 | 106.5 | 150.9 | - | - |
F6 | 35.8 | 267.1 | 107.5 | - | - |
F7 | 122.6 | 107.9 | 102.4 | 80.8 | - |
F8 | 41 | 196.8 | - | 131.8 | - |
F9 | 32.7 | 84.9 | - | 127.1 | - |
平均 | 63.6 | 120.3 | 124.0 | 150.4 | 0 |
Tab. 3
Fault growth rates along line 3"
断层 | 活动速率/(m·Myr-1) | ||||
---|---|---|---|---|---|
56—38Ma | 38—33.9Ma | 33.9—23Ma | 23—16Ma | 16—0Ma | |
F1 | 23.7 | 56.5 | - | - | - |
F2 | 10.8 | 98.5 | 16.4 | 37.7 | - |
F3 | - | 45.8 | - | - | - |
F4 | 10.6 | 47.9 | - | - | - |
F5 | 16.9 | 32.7 | 17 | - | - |
F6 | 14.8 | 99.4 | - | - | - |
F7 | - | 38.1 | - | - | - |
F8 | 45 | 62 | 13.2 | - | - |
F9 | 197 | 88.9 | - | - | - |
F10 | - | - | - | 18.9 | - |
F11 | 49.3 | 33 | 11.5 | 10.9 | - |
F12 | 14.9 | - | - | 12.7 | - |
F13 | 13.2 | - | - | - | - |
F14 | 13.6 | - | 10.3 | - | - |
F15 | - | 11 | - | - | - |
平均 | 37.3 | 55.8 | 13.7 | 20 | 0 |
Tab. 4
Fault growth rates along line 4"
断层 | 活动速率/(m·Myr-1) | |||||
---|---|---|---|---|---|---|
56—38Ma | 38—33.9Ma | 33.9—23Ma | 23—16Ma | 16—10Ma | 10—0Ma | |
F1 | - | 111.4 | 68.4 | 66.7 | 21.8 | - |
F2 | 44 | 179.4 | 77.6 | - | 11.7 | - |
F3 | - | 45.9 | - | - | 4.9 | - |
F4 | 70 | 144.9 | 25.9 | 14 | 59.6 | - |
F5 | 157.1 | 363.8 | 19.6 | - | 38.7 | - |
F6 | 84.6 | 86.6 | 7.6 | - | - | - |
F7 | 66.5 | 221 | 12.8 | - | - | - |
F8 | 29.9 | 327.8 | - | - | - | - |
F9 | 21.2 | 613.8 | - | - | - | - |
平均 | 67.6 | 232.7 | 30.3 | 40.4 | 27.3 | 0 |
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