Oil & Gas Geology ›› 2023, Vol. 44 ›› Issue (3): 565-583.doi: 10.11743/ogg20230304
• Petroleum Geology • Previous Articles Next Articles
Hao LIU1(), Changgui XU2, Yangdong GAO3, Heming LIN3, Xinwei QIU3, Yongtao JU4, Xudong WANG3, Lei LI5, Jun MENG1, Xiaoming QUE3
Received:
2023-02-09
Revised:
2023-04-16
Online:
2023-06-01
Published:
2023-06-05
CLC Number:
Hao LIU, Changgui XU, Yangdong GAO, Heming LIN, Xinwei QIU, Yongtao JU, Xudong WANG, Lei LI, Jun MENG, Xiaoming QUE. Source-to-sink system and hydrocarbon source rock prediction of underexplored areas in rifted lacustrine basins: A case study on northern lows in Zhu Ⅰ Depression, Pearl River Mouth Basin[J]. Oil & Gas Geology, 2023, 44(3): 565-583.
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Table 1
Comprehensive comparison of geologic factors for hydrocarbon source rock development in areas with mature exploration degree and areas with low exploration degree in northern Zhu Ⅰ Depression"
评价要素 | 成熟洼陷 | 低勘探洼陷 | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
LF22 | HZ10 | HZ8 | HF33 | LF7 | HZ11 | HZ5 | ||||||||||
上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | 上文昌组 | 下文昌组 | |
洼陷面积/km2 | 180 ~ 320 | 210 | 350 | 118 | 114 | 58 | 100 | 250 | 190 | 197 | 154 | 94 | 26 | 110 | 9 | |
构造沉降量/m | 450 ~ 1 900 | 740 | 1 900 | 500 | 1 800 | 588 | 1 300 | 1 550 | 950 | 350 | 1 026 | 350 | 266 | 346 | 260 | |
可容空间/km3 | 99 ~ 450 | 150 | 670 | 67 | 204 | 105 | 157 | 170 | 690 | 78 | 160 | 33 | 7 | 38 | 2 | |
A/S | ≥1 | ≥1 | ≥1 | ≥1 | ≤1 | ≤1 | ≥1 | ≥1 | ≥1 | |||||||
母岩类型 | 火成岩、变质岩和沉积岩 | 火成岩为主 | ||||||||||||||
泥岩厚度/m | 100 ~ 700 | 100 ~ 300 | 150 ~ 500 | 90 ~ 380 | 100 ~ 510 | 90 ~ 380 | 100 ~ 400 | 100 ~ 200 | 200 ~ 300 | 100 ~ 200 | 200 ~ 300 | <100 | <100 | <100 | <100 | |
水环境 | 缺氧、富营养 | 缺氧、淡水 | 较富营养 | 缺氧、 富营养 | 较富营养 | 缺氧、 富营养 | 富营养 | 缺氧、 富营养 | 缺氧、富营养 | 缺氧、淡水 | 缺氧、富营养 | |||||
地震相 类型 | SF 1, SF2,SF3, SF4 | SF1 | SF2 | SF4 | SF3 | SF1, SF4 | SF4 | SF4 | SF4 | SF4 | ||||||
沉积相类型 | 滨浅湖-深湖 | 深湖 | 深湖 | 深湖-半深湖 | 深湖-半深湖 | 滨浅湖 | 深湖 | 深湖-半深湖 | 深湖-半深湖 | |||||||
烃源岩发育条件 | Ⅰ | Ⅰ | Ⅱ | Ⅰ | Ⅱ | Ⅰ | Ⅱ | Ⅱ | Ⅲ | Ⅰ | Ⅲ | Ⅲ | Ⅲ | Ⅲ |
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