Earth Science Frontiers ›› 2023, Vol. 30 ›› Issue (1): 81-105.DOI: 10.13745/j.esf.sf.2022.8.35
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HE Bizhu1,2(), ZHENG Menglin3, YUN Xiaorui1,4,5, CAI Zhihui1, JIAO Cunli5, CHEN Xijie1,6, ZHENG Yong1,2, MA Xuxuan1,2, LIU Ruohan1,7, CHEN Huiming1, ZHANG Shengsheng8, LEI Min1, FU Guoqiang9, LI Zhenyu1,4
Received:
2022-07-07
Revised:
2022-08-05
Online:
2023-01-25
Published:
2022-10-20
CLC Number:
HE Bizhu, ZHENG Menglin, YUN Xiaorui, CAI Zhihui, JIAO Cunli, CHEN Xijie, ZHENG Yong, MA Xuxuan, LIU Ruohan, CHEN Huiming, ZHANG Shengsheng, LEI Min, FU Guoqiang, LI Zhenyu. Structural architecture and energy resource potential of Gonghe Basin, NE Qinghai-Tibet Plateau[J]. Earth Science Frontiers, 2023, 30(1): 81-105.
Fig.1 Geological sketch map of Gonghe Basin and its adjacent area in Qinghai Province,NE Qinghai-Tibet Plateau.A and B modified after [42,46-47]; C modified after [46⇓⇓-49].
Fig.2 Comprehensive column of the Gonghe Basin and its adjacent area from Mesozoic to Cenozoic,NE Qinghai-Tibet Plateau. Modified after [38-39,46⇓⇓-49,81-82].
地层 | 岩性 | 密度/(g·cm-3) | 磁化率K/ (4π× 10-6SI) | 剩余磁化强度 Jr/(10-3A· m-1) | 电阻率/(Ω·m) | 速度/(m·s-1) | 位置 | |||
---|---|---|---|---|---|---|---|---|---|---|
范围 | 平均值 | 范围 | 平均值 | 范围 | 平均值 | |||||
第四系 | 砂岩、粉砂岩 | 1.59~2.08 | 1.8 | n×10 | 8~50 | 16 | 1 600~2 860 | 2 400 | GR1井 测井及 岩心实测 | |
新近系 | 砂岩、泥岩 | 1.71~2.26 | 2.23 | n | 5~25 | 12 | 1 550~3 580 | 2 600 | ||
古近系 | 砾岩、砂岩 | 1.91~2.45 | n×10 | 12~22 | 17 | 200~4 660 | 3 030 | |||
白垩系 | 砾岩、砂岩 | 2.54~2.68 | 2.61 | 无磁性 | 盆地 周缘 露头 | |||||
安山岩、橄榄玄武岩 | 180~3 070 | 450~4 950 | ||||||||
侏罗系 | 砂岩 | 2.46~2.62 | 2.56 | 无磁性 | ||||||
安山岩 | 500~2 500 | 180~2 100 | ||||||||
三叠系 | 砂岩、砾岩、灰岩、板岩 | 2.43~2.69 | 2.61 | n×102 | n×102 | 盆地 周缘 露头 | ||||
安山岩、火山角砾岩、 板岩、灰岩 | 2.54~2.8 | 2.66 | 500~2 500 | 180~2 100 | ||||||
花岗岩、花岗闪长岩 | 2.50~2.72 | 2.63 | 500~4 700 | n×10~2 700 | 25~50 | 35 | 4 550~6 660 | 5 880 | GR1井 测井及 岩心实测 | |
蚀变花岗闪长岩 | 8~38 | 18 | 2 700~5 880 | 3 800 | ||||||
前三 叠系 | 浅变质岩、千枚岩、 板岩、片岩、片麻岩 | 2.41~2.94 | 2.65 | n×102~ 7 800 | n×102~n×103 | |||||
火成岩 | 2.5~3.10 | 2.71 | 300~7 000 | 160~2 700 | 盆地 周缘 露头 |
Table 1 The density and magnetic parameters of rocks in the periphery area of the Gonghe Basin
地层 | 岩性 | 密度/(g·cm-3) | 磁化率K/ (4π× 10-6SI) | 剩余磁化强度 Jr/(10-3A· m-1) | 电阻率/(Ω·m) | 速度/(m·s-1) | 位置 | |||
---|---|---|---|---|---|---|---|---|---|---|
范围 | 平均值 | 范围 | 平均值 | 范围 | 平均值 | |||||
第四系 | 砂岩、粉砂岩 | 1.59~2.08 | 1.8 | n×10 | 8~50 | 16 | 1 600~2 860 | 2 400 | GR1井 测井及 岩心实测 | |
新近系 | 砂岩、泥岩 | 1.71~2.26 | 2.23 | n | 5~25 | 12 | 1 550~3 580 | 2 600 | ||
古近系 | 砾岩、砂岩 | 1.91~2.45 | n×10 | 12~22 | 17 | 200~4 660 | 3 030 | |||
白垩系 | 砾岩、砂岩 | 2.54~2.68 | 2.61 | 无磁性 | 盆地 周缘 露头 | |||||
安山岩、橄榄玄武岩 | 180~3 070 | 450~4 950 | ||||||||
侏罗系 | 砂岩 | 2.46~2.62 | 2.56 | 无磁性 | ||||||
安山岩 | 500~2 500 | 180~2 100 | ||||||||
三叠系 | 砂岩、砾岩、灰岩、板岩 | 2.43~2.69 | 2.61 | n×102 | n×102 | 盆地 周缘 露头 | ||||
安山岩、火山角砾岩、 板岩、灰岩 | 2.54~2.8 | 2.66 | 500~2 500 | 180~2 100 | ||||||
花岗岩、花岗闪长岩 | 2.50~2.72 | 2.63 | 500~4 700 | n×10~2 700 | 25~50 | 35 | 4 550~6 660 | 5 880 | GR1井 测井及 岩心实测 | |
蚀变花岗闪长岩 | 8~38 | 18 | 2 700~5 880 | 3 800 | ||||||
前三 叠系 | 浅变质岩、千枚岩、 板岩、片岩、片麻岩 | 2.41~2.94 | 2.65 | n×102~ 7 800 | n×102~n×103 | |||||
火成岩 | 2.5~3.10 | 2.71 | 300~7 000 | 160~2 700 | 盆地 周缘 露头 |
样品位置 | 地层时代 | 深度/m | 岩性 | 生热率/(μW·m-3) | 资料来源 | ||
---|---|---|---|---|---|---|---|
样品数 | 范围 | 平均值 | |||||
GR1 | Cz | 沉积岩 | 4 | 1.66~2.02 | 1.79 | 文献[106] | |
GR1 | T | 花岗岩 | 20 | 1.73~4.48 | 3.04 | ||
GR2 | Cz | 沉积岩 | 3 | 1.21~1.90 | 1.5 | ||
GR2 | T | 花岗岩 | 20 | 1.17~4.92 | 2.98 | ||
DR3 | T | 花岗岩 | 5 | 2.12~5.81 | 4.7 | ||
ZR2 | Cz | 沉积岩 | 5 | 1.83~2.40 | 2.13 | ||
ZR2 | T | 花岗岩 | 41 | 0.92~6.49 | 2.81 | ||
贵德 | 0~1 500 | 沉积岩 | 10 | 1.88 | 文献[107] | ||
T | 1 500~3 000 | 花岗岩 | 14 | 2.04 | |||
HDR3 | T | 2 391~2 392 | 细晶花岗岩脉 | 2 | 6.17~6.87 | 6.52 | 本研究 |
HDR3 | T | 2 617~2 633 | 钾长花岗岩 | 3 | 7.28~7.57 | 7.36 | |
HDR3 | T | 1 710~1 711 | 高镁闪长岩 | 3 | 0.97~1.01 | 0.98 | |
HDR3 | T | 1 607~1 614 | 花岗闪长岩 | 6 | 2.25~2.74 | 2.46 | |
5LYX-9 | T | 露头 | 石英闪长岩 | 5 | 0.73~1.03 | 0.96 | |
5LYX-9-5 | T | 露头 | 辉長岩 | 10 | 0.47~0.76 | 0.59 | |
DR6-DR10 | Cz | 490~1 560 | 细砂岩 | 13 | 0.79~1.65 | 1.33 | |
DR6-DR10 | Cz | 281~1 533 | 粉砂岩 | 16 | 0.92~2.53 | 1.72 |
Table 2 The radiogenic heat generation rate and velocity of rocks in the Gonghe Basin and its periphery area
样品位置 | 地层时代 | 深度/m | 岩性 | 生热率/(μW·m-3) | 资料来源 | ||
---|---|---|---|---|---|---|---|
样品数 | 范围 | 平均值 | |||||
GR1 | Cz | 沉积岩 | 4 | 1.66~2.02 | 1.79 | 文献[106] | |
GR1 | T | 花岗岩 | 20 | 1.73~4.48 | 3.04 | ||
GR2 | Cz | 沉积岩 | 3 | 1.21~1.90 | 1.5 | ||
GR2 | T | 花岗岩 | 20 | 1.17~4.92 | 2.98 | ||
DR3 | T | 花岗岩 | 5 | 2.12~5.81 | 4.7 | ||
ZR2 | Cz | 沉积岩 | 5 | 1.83~2.40 | 2.13 | ||
ZR2 | T | 花岗岩 | 41 | 0.92~6.49 | 2.81 | ||
贵德 | 0~1 500 | 沉积岩 | 10 | 1.88 | 文献[107] | ||
T | 1 500~3 000 | 花岗岩 | 14 | 2.04 | |||
HDR3 | T | 2 391~2 392 | 细晶花岗岩脉 | 2 | 6.17~6.87 | 6.52 | 本研究 |
HDR3 | T | 2 617~2 633 | 钾长花岗岩 | 3 | 7.28~7.57 | 7.36 | |
HDR3 | T | 1 710~1 711 | 高镁闪长岩 | 3 | 0.97~1.01 | 0.98 | |
HDR3 | T | 1 607~1 614 | 花岗闪长岩 | 6 | 2.25~2.74 | 2.46 | |
5LYX-9 | T | 露头 | 石英闪长岩 | 5 | 0.73~1.03 | 0.96 | |
5LYX-9-5 | T | 露头 | 辉長岩 | 10 | 0.47~0.76 | 0.59 | |
DR6-DR10 | Cz | 490~1 560 | 细砂岩 | 13 | 0.79~1.65 | 1.33 | |
DR6-DR10 | Cz | 281~1 533 | 粉砂岩 | 16 | 0.92~2.53 | 1.72 |
Fig.10 Stress mechanisms during the formation of the Gonghe Basin. Fault deformation ages and properties adapted from: [8-9],①;[88],②;[109],③;[110],④;[89-90],⑤;[95],⑥;[97],⑦;[111],⑧;[112],⑨;[113],⑩;[30],⑪.
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