Southwestern Provenance-Sedimentary System and Provenance Tectonic Setting of Eastern Sag in the North Yellow Sea Basin
-
摘要: 物源-沉积体系是原始储层物性的主要影响因素，与源区构造背景的综合分析是油气勘探工作的基础.北黄海盆地是位于苏鲁造山带-临津江造山带北侧中朝板块上中-新生代转换伸展断陷盆地.地震和钻井资料证实东部坳陷西南部有中-上侏罗统三角洲砂体发育.岩心和测井上可识别的沉积类型包括分流河道、决口扇、河口坝和远砂坝等，地震反射结构显示出来自西南方向的沉积物进积.砂岩样品的岩矿组成显示，碎屑中存在花岗质成分和酸性火山岩成分.泥岩元素地球化学特征显示其物质成分以长英质为主，推测源区为克拉通或再旋回造山带.砂岩Dickinson图解表明，不仅存在来自克拉通或再旋回造山带的成分，而且存在火山弧造山带的成分.综合分析认为，北黄海盆地东部坳陷西南物源区为再旋回造山带，花岗质成分来自西南盆缘的基底花岗质岩石的风化，而火山岩成分可能是同期火山喷发的产物，也可能是先前火山岩的风化产物.Abstract: The comprehensive analysis of provenance-sedimentary system and provenance tectonic setting is the basis of oil and gas exploration, the provenance-sedimentary system is the main influence factor of the original reservoir. The North Yellow Sea basin is a Mesozoic-Cenozoic transtensional faulted basin located between Sulu-Linjinjiang orogeny and Jiao-Liao uplift. The delta sand deposits developed during the Middle-Late Jurassic have been confirmed by seismic and drilling data in the southwest of eastern sag, the North Yellow Sea basin. Some sedimentary types, including distributary channel, crevasse splay, mouth bar and distal bar, can be recognized in the core rocks and well loggings, and the progradation of sediments in northwestern orientation is shown in the seismic reflection. The analysis of petrology and mineralogy of the sandstone samples indicate that they contain granitic and acid volcanic compositions. The element geochemistry characteristics of the mudstone samples show that their major composition is felsic, and the provenance is the craton or the recycling orogeny. The Dickinson diagram of the sands demonstrates their compositions coming from both the craton or the recycling orogeny and volcanic arc orogeny. We suggest that the southwestern provenance in the eastern sag of the North Yellow Sea basin is the recycling orogeny. The granitic composition comes from the weathered basement granitic rocks, and the volcaniclastics may come from the syn-eruption, or from weathered pre-existing volcanic rocks.
-
图 2 北黄海盆地东部坳陷中-上侏罗统过B2和B3井地震解释剖面
a.整个构造-地层解释剖面；b.部分地震剖面；c.部分解释剖面
Fig. 2. The Seismic profile and its interpretation of the middle-upper Jurassic of the eastern sag in the North Yellow Sea basin with Well B2 and Well B3
图 3 北黄海盆地东部坳陷中-上侏罗统盆地充填序列
LST.低位体系域；EST.湖扩体系域；HST.高位体系域
Fig. 3. The middle-upper Jurassic filling succession of the Eastern sag, the North Yellow Sea basin
图 5 典型沉积微相特征
a.B3井3 093.20~3 093.36 m井段(J3)，分流河道，4个向上变细的正韵律；b.B3井3 090.78~3 090.88 m井段(J3)，决口扇，砂泥混杂，波状层理；c.B3井3 091.06~3 091.18 m井段(J3)，决口扇，砂泥混杂；d.B3井3 093.12 m井段(J3)，沼泽；e.B3井3 212.64~3 212.70 m井段(J2)，静水泥，含泥砾；f.B2井2 727.55~2 727.71 m井段(J3)，远砂坝，透镜状层理；g.B2井2 955.90~2 956.00 m井段(J3)，河口坝，斜层理；h.B2井2 956.43~2 956.57 m井段(J3)，河口坝；i.B3井3 208.07~32 08.15 m井段(J2)，浊流，薄层状发育
Fig. 5. Characteristics of typical sedimentary microfacies
图 6 物质成分特征
a~i.时代均为J3；a.样品B2-6(2 955.18~2 955.20 m)为花岗岩屑；b.样品B2-5(2 955.02~2 955.05 m)为花岗岩屑；c.样品B2-9(2 957.28~2 957.33 m)为流纹岩屑；d.样品B2-1(2 730.29~2 730.31 m)为火山炸裂晶屑；e.样品B2-9(2 957.28~2 957.33 m)为石英熔蚀；f.样品B2-5(2 955.02~2 955.05 m)为正长石；g.样品B3-2(3 094.32~3 094.38 m)，其中① 低温石英、② 高温石英/凝灰质基质；h.样品B2-7(2 955.62~2 955.64 m)，其中① 低温石英、② 高温石英/凝灰质基质；i.样品B3-1(3 094.62~3 094.66 m)为凝灰质基质；j.样品B2-8(2 955.98~2 956.00 m)，其中① 长石、② 粘土质(伊利石)；k.样品B2-7(2 955.62~2 955.64 m)为石英；l.样品B3-2(3 094.32~3 094.38 m)，其中① 石英、② 粘土质(高岭石)
Fig. 6. Characteristics of material compositions
图 7 中-上侏罗统主量元素构造环境判别图解
a, b.底图据Bhatia(1983)；c.底图据Roser and Korsch(1986)；A.大洋岛弧；B.大陆岛弧；C.活动大陆边缘；D.被动大陆边缘
Fig. 7. Major elements composition plots of the upper-middle Jurassic mudstones for tectonic setting discrimination
图 8 中、上侏罗统Ni-TiO2(a)、La/Th-Hf(b)和碎屑岩源区主元素判别图解(c)
a底图据Floyd et al.(1989)；b底图据Taylor and McLennan(1985)；c底图据Roser and Korsch(1988)；P1.镁铁质的和少量中性火成岩源区；P2.主要中性火成岩源区(主要为安山岩)；P3.长英质火成岩源区(大陆边缘弧)；P4.古老的沉积体系或克拉通/再旋回造山带
Fig. 8. Ni-TiO2、Hf-La/Th and provenance discriminant function plots of the upper-middle Jurassic
图 9 上侏罗统Dickinson图解
底图据Dickinson and Sucaek(1979)；黑色方块代表B2井样品；灰色三角形代表B3井样品
Fig. 9. The Dickinson diagram of the upper Jurassic
图 10 东部坳陷中-上侏罗统西南沉积体系发育模式
Fig. 10. Model of the southwest sedimentary system of the upper-middle Jurassic in the Eastern sag
表 1 碎屑组分含量(%)
Table 1. The percentage content of clastic component
井 样品 深度(m) 定名 Qp Qm P K R T G Ls Tu Ca B2 B2-1 2 730.29 凝灰质含钙岩屑石英细砂岩 2 42 0 5 12 5 8 3 15 8 B2-2 2 952.61 钙质凝灰质岩屑粗砂岩 20 31 0 2 14 2 4 5 4 19 B2-3 2 954.04 凝灰质岩屑石英含砾粗砂岩 45 22 0 2 5 4 7 1 13 1 B2-4 2 954.19 岩屑石英含砾粗砂岩 25 27 0 6 8 4 18 0 9 3 B2-5 2 955.02 岩屑石英含砾粗砂岩 32 41 0 2 9 2 5 1 7 3 B2-7 2 955.62 凝灰质岩屑石英含砾粗砂岩 19 43 1 6 11 6 5 2 5 4 B2-8 2 955.98 岩屑石英中砂岩 11 58 2 0 8 3 3 2 9 4 B2-9 2 957.28 岩屑石英中砂岩 14 58 0 1 10 3 2 2 9 2 B3 B3-6 3 091.43 含钙岩屑石英粗砂岩 20 45 0 3 9 0 14 0 0 9 B3-3 3 093.54 岩屑石英含砾粗砂岩 28 50 0 1 5 0 9 0 3 5 B3-2 3 094.32 岩屑石英含砾中粗砂岩 36 45 0 1 5 3 8 0 3 0 注：Qp.多晶石英；Qm.单晶石英；P.斜长石；K.正长石；R.流纹岩屑；T.凝灰岩屑；G.花岗岩屑；Ls.沉积岩屑；Tu.凝灰质基质；Ca.钙质. 
下载: 导出CSV
表 2 北黄海盆地东部坳陷中-下侏罗统泥岩样品的主量(%)、微量及稀土元素含量(10-6)(B3井)
Table 2. The contents of major elements, trace elements and rare-earth elements of the middle-upper Jurassic mudstones of Eastern sag in the North Yellow Sea basin (Well B3)
样号 上侏罗统 中侏罗统 B3-4 B3-5 B3-7 B3-8 B3-9 B3-10 B3-11 B3-12 B3-13 SiO2 48.78 57.36 55.58 54.10 52.40 53.52 58.82 49.20 51.20 Al2O3 21.95 15.23 18.44 16.90 15.50 16.43 17.70 15.91 16.29 Fe2O3 1.51 0.37 1.65 1.47 2.31 2.23 1.92 2.52 1.52 FeO 6.87 0.41 5.60 3.52 5.64 3.68 1.72 6.87 3.89 TiO2 1.10 0.76 0.84 0.70 0.66 0.80 0.72 0.66 0.70 P2O5 0.15 0.15 0.20 0.15 0.25 0.25 0.20 0.40 0.45 MnO 0.08 0.02 0.06 0.10 0.18 0.12 0.03 0.22 0.14 CaO 0.49 0.35 0.51 3.11 2.75 3.46 1.65 2.97 4.26 MgO 2.66 0.33 2.12 2.99 3.00 2.96 1.62 2.88 3.36 K2O 2.610 2.310 1.890 4.570 4.500 4.680 5.100 4.420 4.820 Na2O 0.10 0.06 0.08 1.28 0.95 0.92 0.86 1.39 0.74 LOI 13.37 22.46 12.46 10.70 11.48 10.71 9.26 12.42 12.45 Total 92.8 99.4 93.83 96.07 93.98 96.08 97.88 92.99 95.93 Fe2O3T 8.38 0.78 7.25 4.99 7.95 5.91 3.64 9.39 5.41 SiO2/Al2O3 2.22 3.77 3.01 3.20 3.38 3.26 3.32 3.09 3.14 K2O/Na2O 26.10 38.50 23.63 3.57 4.74 5.09 5.93 3.18 6.51 Al2O3/TiO2 19.95 20.04 21.95 24.14 23.48 20.54 24.58 24.11 23.27 Fe2O3+MgO 4.17 0.70 3.77 4.46 5.31 5.19 3.54 5.40 4.88 Al2O3/SiO2 0.45 0.27 0.33 0.31 0.30 0.31 0.30 0.32 0.32 Al2O3/(CaO+NaO) 37.20 37.15 31.25 3.85 4.19 3.75 7.05 3.65 3.26 K2O+Na2O 2.71 2.37 1.97 5.85 5.45 5.60 5.96 5.81 5.56 Ni 135.90 63.46 88.24 36.54 25.28 23.69 51.10 29.82 28.70 Hf 4.560 7.198 7.215 8.035 7.732 8.342 9.029 7.799 7.955 La 207.80 63.46 117.40 84.33 83.00 83.59 94.69 76.50 77.02 Th 24.8 16.3 19.1 25.3 23.6 26 26.6 23.4 24.4 Cr 141.8 80.18 140.6 79.18 71.85 76.16 87.30 70.80 74.00 Zr 160.6 281.8 270.3 310.0 305.9 332.7 342.4 309.5 315.8 Cr/Zr 0.88 0.28 0.52 0.26 0.23 0.23 0.25 0.23 0.23 La/Th 8.39 3.90 6.14 3.33 3.52 3.22 3.55 3.27 3.16
下载: 导出CSV
表 3 碎屑岩源区性质判别函数的变量组成及其系数
Table 3. Provenance discriminant function coefficients used to calculate discriminant scores for clastic rocks
变量 TiO2 Al2O3 Fe2O3T MgO CaO Na2O K2O 常量C F1系数 -1.773 0.607 0.760 -1.500 0.616 0.509 -1.224 -9.090 F2系数 0.445 0.070 -0.250 -1.142 0.438 1.475 1.426 -6.681 注：判别公式为F=a1x1+a2x2+…+anxn+C，其中，x1~xn为n个判别变量，a1~an为其相应系数；据Roser and Korsch(1988).
下载: 导出CSV
表 4 Dickinson图解各组分含量(%)
Table 4. The contents of components used in Dickinson diagram
井号 样品号 顶深(m) 底深(m) 定名 Q F L Qm F Lt Qp Lv Ls Qm P K B2 B2-1 2 730.29 2 730.31 细砂岩 74.58 7.76 17.66 71.37 7.76 20.88 15.40 84.60 0 90.20 0.78 9.02 B2-2 2 952.61 2 952.64 粗砂岩 67.86 1.54 30.6 40.36 1.54 58.10 47.33 50.05 2.62 96.33 0 3.67 B2-3 2 954.04 2 954.05 粗砂岩 71.86 1.61 26.54 23.86 1.61 74.53 64.40 34.16 1.44 93.68 0 6.32 B2-4 2 954.19 2 954.20 粗砂岩 41.08 4.65 54.27 21.64 4.65 73.71 26.38 70.82 2.81 82.31 0 17.69 B2-5 2 955.02 2 955.05 粗砂岩 79.46 2.09 18.45 44.71 2.09 53.20 65.32 30.48 4.21 95.54 1.01 3.45 B2-7 2 955.62 2 955.64 粗砂岩 75.61 7.02 17.37 52.31 7.02 40.66 57.28 39.13 3.59 88.16 1.14 10.70 B2-8 2 955.98 2 956.00 中砂岩 80.53 1.72 17.75 67.28 1.72 31.00 42.76 55.74 1.50 97.51 2.49 0 B2-9 2 957.28 2 957.33 中砂岩 80.01 1.38 18.61 64.38 1.38 34.25 45.65 48.50 5.84 97.91 0 2.09 B3 B3-2 3 094.32 3 094.38 粗砂岩 84.81 0.70 14.50 46.46 0.70 52.85 72.57 21.35 6.08 98.52 0.00 1.48 B3-3 3 093.54 3 093.60 粗砂岩 82.05 0.00 17.95 53.50 0.00 46.50 61.40 29.17 9.43 100.00 0.00 0.00 B3-6 3 091.43 3 091.47 粗砂岩 80.53 3.05 16.42 55.19 3.05 41.76 60.67 29.94 9.39 94.76 0.00 5.24 注：Q.稳定石英颗粒，其中包括Qm和Qp；Qm.单晶石英颗粒；Qp.复晶石英颗粒，主要为燧石质颗粒；F.单晶长石颗粒，其中包括P和K；P.斜长石单晶颗粒；K.钾长石单晶颗粒；L.不稳定复晶岩屑，其中包括Lv和Ls；Lv.火山岩屑和变质火山岩屑；Ls.沉积岩屑和变质沉积岩屑；Lt.岩屑总含量，即相当于L与Qp之和.
下载: 导出CSV
-
Bhatia, M.R., 1983.Plate Tectonics and Geochemical Composition of Sandstones.Journal of Geology, 91(6):611-627.doi: 10.1086/628815 Cai, F., Sun, P., 2006.Sino-Korean Orogenic Belt and Sedimentary Basin in the Yellow Sea.Marine Sciences, 30(7):69-75 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYKX200607016.htm Cai, Q.Z., 2002.Regional Geology and Geotectonic Environment of Petroliferous Basins in the Yellow Sea.Marine Geology Letters, 18(11):8-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HYDT200211004.htm Cai, Q.Z., 2005.Relationship between Sino-Korean Orogenic Belt Traversing Yellow Sea and Basin Evolution and Hydrocarbon Generation in North and South Yellow Sea Basins.Oil & Gas Geology, 26(2):185-192, 196 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200502009.htm Chen, L., Bai, Z.L., Li, W.Y., 2006.The Character of Mid-Cenozoic Sedimental Depression and Oil-Gas Exploration Direction in North Yellow Sea.Geophysical Prospecting for Petroleum, 45(3):319-323 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SYWT200603021.htm Chen, L., Jin, Q.H., Liu, Z.H., et al., 2008.Features and Genetic Mechanism of Faults in the Sun Basin in Mesozoic and Cenozoic Times.Marine Geology & Quaternary Geology, 28(2):53-60 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-hydz200802015.htm Cheng, R.H., Li, F., Shen, Y.J., et al., 2011.The Seismic Reflection Features of Volcanic Stratum and the Seismic-Geological Interpretation:The Case Study in Xujiaweizi Faulted Depression, Songliao Basin.Chinese Journal of Geophysics, 54(2):611-619 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQWX201102042.htm Dickinson, W.R., Sucaek, C.A., 1979.Plate Tectonics and Sandstone Compositions.AAPG Bulletin, 63(12):2164-2182.doi: 10.1306/2F9188FB-16CE-11D7-8645000102C1865D Du, M., Hu, X.Q., Wang, G.Y., 2014a.Sequence Stratigraphic Characteristics and Depositional Systems in the Southeast of the Eastern Depression of the North Yellow Sea Basin.Marine Geology Frontiers, 30(1):25-33 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HYDT201401004.htm Du, M., Wang, G.Y., Liu, J.P., et al., 2014b.Stratigraphic Delinestion and Depositional Characteristics in the Eastern Depression, North Yellow Sea Basin.Special Oil and Gas Reservoirs, 21(2):51-56(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-TZCZ201402011.htm Einsele, G., 2000.Sedimentary Basins:Evolution, Facies and Sediment Budge.Springer, Berlin, 3-10. Fisher, R.V., Schmincke, H.U., 1984.Pyroclastic Rocks.Springer-Verlag, Heideberg, New York, Berlin, 247-256. Floyd, P.A., Winchester, J.A., Park, R.G., 1989.Geochemistry and Tectonic Setting of Lewisian Clastic Metasediments from the Early Proterozoic Loch Maree Group of Gairloch, NW Scotland.Precambrian Research, 45(1):203-214.doi:10.1016/0301-9268(89) 90040-5 Gao, S.L., Zhou, Z.Y., Wang, L.L., 2014.Zircon U-Pb Dating and Geological Significance for Jurassic Igneous Rocks in North Yellow Sea Basin.Journal of Tongji University (Natural Science), 42(3):480-487 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-TJDZ201403024.htm Girty, G.H., Ridge, D.L., Knaack, C., et al., 1996.Provenance and Depositional Setting of Paleozoic Chert and Argillite, Sierra Nevada, California.Journal of Sedimentary Research, 66(1):107-118.doi: 10.1306/D42682CA-2B26-11D7-8648000102C1865D He, J.Q., Liang, S.Y., Zhao, Y.Q., et al., 2007.Characteristics of Geologic Structures of the North Yellow Sea Basin:Implications for Petroleum Exploration.Marine Geology & Quaternary Geology, 27(2):101-105 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200702017.htm Hu, X.Q., Liu, Z.H., Chen, L., et al., 2009.Cycle Sequence Stratigraphy and Sedimentary Characteristics of Study Area X in the North Yellow Sea Basin.Marine Geology & Quaternary Geology, 29(2):103-110 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-hydz200902018.htm Lechler, P.J., Desilets, M.O., 1987.A Review of the Use of Loss on Ignition as a Measurement of Total Volatiles in Whole Rock Analysis.Chemical Geology, 63(3-4):341-344.doi: 10.1016/0009-2541(87)90171-9 Li, H.Y., 1983.On the Characteristics of Cathodoluminescence of Quartz and Its Application to Sandstone Petrology.Acta Sedimentologica Sinica, 1(2):166-171 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB198302013.htm Li, L., Yao, G.Q., Liu, Y.H., et al., 2015.Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China.Earth Science, 40(9):1480-1496(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201509003.htm Li, S.T., Pan, Y.L., Lu, Y.C., et al., 2002.Key Technology of Prospecting and Exploration of Subtle Traps in Lacustrine Fault Basins:Sequence Stratigraphic Researches on the Basis of High Resolution Seismic Survey.Earth Science, 27(5):592-598 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200205018.htm Li, S.Z., Yu, S., Zhao, S.J., et al., 2013.Tectonic Transition and Plate Reconstruction of the East Asian Continental Margin.Marine Geology & Quaternary Geology, 33(3):65-94 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ201303011.htm Li, W.Y., Li, D.X., Xia, B., et al., 2006.Characteristics of Structural Evolution in North Yellow Sea Basin.Geoscience, 20(2):268-276 (in Chinese with English abstract). https://www.researchgate.net/publication/284685844_Characteristics_of_structural_evolution_in_North_Yellow_Sea_Basin Li, W.Y., Zeng, X.H., Wang, X.G., et al., 2009.Analysis of Structural Kinematics of North Yellow Sea Basin.Earth Science Frontiers, 16(4):74-86 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200904010.htm Lin, C.S., 2006.Tectono-Stratigraphic Analysis of Sedimentary Basins:A Case Study on the Inland Tectonically Active Basind in China.Geoscience, 20(2):185-194 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ200602000.htm Liu, J.P., Wang, G.Y., Du, M., et al., 2013.Analyzing Characteristics of Mesozoic Hydrocarbon Source Rocks in the Eastern Depression, North Yellow Sea Basin.China Offshore Oil and Gas, 25(4):12-16 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZHSD201304003.htm Liu, Z.H., Gao, H.F., Hu, X.Q., et al., 2007.A Study on the Mesozoic Petroleum System in East Depression, North Yellow Sea Basin.China Offshore Oil and Gas, 19(4):229-233 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD200704002.htm Liu, Z.H., Wang, F.Y., Liu, J.P., et al., 2014.Time of Hydrocarbon Accumulation in Eastern Depression of North Yellow Sea Basin.Petroleum Geology & Experiment, 36(5):550-554 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SYSD201405007.htm Liu, Z.T., Yu J.Q., Zheng, B.H., et al., 2006.Application of Loss on Ignition to the Study of Lake Sediments and Environmental Changes.Journal of Salt Lake Research, 14(2):67-72 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YHYJ200602013.htm Ma, W.T., Yu, W.H., Zhang, S.H., 2005.The Structural Features of North Yellow Sea Basin and Its Evolution.Marine Geology Letters, 21(11):21-27 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDT200511005.htm Manville, V., Nemeth, K., Kano, K., 2009.Source to Sink:A Review of Three Decades of Progress in the Understanding of Volcaniclastic Processes, Deposits and Hazards.Sedimentary Geology, 220(3):136-161.doi: 10.1016/j.sedgeo.2009.04.022 Mitchum, R.M., Vail, P.R., Sangree, J.B., 1977.Seismic Stratigraphy and Global Changes of Sea Level:Part 6.Stratigraphic Interpretation of Seismic Reflection Patterns in Depositional Sequences:Section 2.Application of Seismic Reflection Configuration to Stratigraphic Interpretation.AAPG Special Volumes, 26:117-133. http://archives.datapages.com/data/specpubs/seismic1/data/a165/a165/0001/0100/0117.htm Pettijohn, F.J., 1963.Chemical Composition of Sandstones, Excluding Carbonate and Volcanic Sands.Geol.Surv.Prof.Pap., Washington, 19. https://www.mendeley.com/research-papers/chemical-composition-sandstones-excluding-carbonate-volcanic-sands-chapter-s/ Roser, B.P., Korsch, R.J., 1986.Determination of Tectonic Setting of Sandstone-Mudstone Suites Using SiO2 Content and K2O/Na2O Ratio.The Journal of Geology, 94(5):635-650.doi: 10.1086/629071 Roser, B.P., Korsch, R.J., 1988.Provenance Signatures of Sandstone-Mudstone Suites Setermined Using Discriminant Function Analysis of Major-Element Data.Chemical Geology, 67(1-2):119-139.doi: 10.1016/0009-2541(88)90010-1 Siever, R., 1979.Plate-Tectonic Controls on Diagenesis.The Journal of Geology, 87(2):127-155.doi: 10.1086/628405 Taylor, S.R., McLennan, S.M., 1985.The Continental Crust:Its Composition and Evolution.Blackwell, Oxford. https://www.osti.gov/scitech/biblio/6582885 Tian, Z, X., Zhang, X.H., Xue, R.J., 2004.Regional Geologic Features of the North Yellow Sea Basin.Marine Geology Letters, 20(2):8-10, 50 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDT200402003.htm Wang, H.J., Wang, L.L., Feng, C.M., 2014.On Dynamic Mechanism of Tectonic Evolution in the North Yellow Sea Basin.Journal of Oil and Gas Technology, 36(5):1-8 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-JHSX201405001.htm Wang, L.L., Shen, Y.J., Cheng, R.H., et al., 2013.Geochemistry and Tectonic Background of Middle-Upper Jurassic Volcanic Rocks in the North Yellow Sea Basin.Journal of Central South University (Science and Technology), 44(1):223-232 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZNGD201301031.htm Wang, L.L., Xu, Z.J., Cheng, R.H., et al., 2015.Zircon U-Pb Geochronology of Early Jurassic-Late Cretaceous Volcanic Rocks in North Yellow Sea Basin.Geotectonica et Metallogenia, 39(1):179-186 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DGYK201501016.htm Wronkiewica, D.J., Condie, K.C., 1989.Geochemistry and Provenance of Sediments from the Pongola Supergroup, South Africa:Evidence for a 3.0-Ga-Old Continental Craton.Geochimica et Cosmochimica Acta, 53(7):1537-1549.doi:10.1016/0016-7037(89) 90236-6 Wu, S.Y., Liu, J., 2015.Characteristics of Milankovitch Cycle in Eocene Formation, Eastern Depression of the North Yellow Sea Basin.Earth Science, 40(11):1933-1944(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DQKX201511016.htm Yuan, S.K., Wang, Y.M., Liu, Z.H., et al., 2010.Unconformity Types and Hydrocarbon Accumulation Models in the Eastern Depression of the North Yellow Sea Basin.Petroleum Exploration and Development, 37(6):663-667 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SKYK201006005.htm Zhang, L., Zhou, Y.Z., Wang, L.L., et al., 2009.A Study on Hydrocarbon Generation Conditions in the North Yellow Sea Basin.Natural Gas Industry, 29(1):21-25, 131-132 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TRQG200901008.htm Zhang, Y.Q., Li, J.L., Zhang, T., et al., 2008.Cretaceous to Paleocene Tectono-Sedimentary Evolution of the Jiaolai Basin and the Contiguous Areas of the Shandong Peninsula (North China) and Its Geodynamic Implications.Acta Geologica Sinica, 82(9):1229-1257 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200809007.htm Zheng, Q.G., Cai, L.G., Ding, W.L., et al., 2005.Development and Evolution of Basins in Yellow Sea.Oil & Gas Geology, 26(5):647-654 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200505016.htm 蔡峰, 孙萍, 2006.黄海海域的中朝造山带与沉积盆地.海洋科学, 30(7):69-75. http://www.cnki.com.cn/Article/CJFDTOTAL-HYKX200607016.htm 蔡乾忠, 2002.黄海含油气盆地区域地质与大地构造环境.海洋地质动态, 18(11):8-12. doi: 10.3969/j.issn.1009-2722.2002.11.005 蔡乾忠, 2005.横贯黄海的中朝造山带与北、南黄海成盆成烃关系.石油与天然气地质, 26(2):185-192, 196. doi: 10.11743/ogg20050208 陈玲, 白志琳, 李文勇, 2006.北黄海盆地中新生代沉积坳陷特征及其油气勘探方向.石油物探, 45(3):319-323. http://www.cnki.com.cn/Article/CJFDTOTAL-SYWT200603021.htm 陈亮, 金庆焕, 刘振湖, 等, 2008.太阳盆地中新生代断裂特征及成因机制.海洋地质与第四纪地质, 28(2):53-60. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200802015.htm 程日辉, 李飞, 沈艳杰, 等, 2011.火山岩地层地震反射特征和地震-地质联合解释:以徐家围子断陷为例.地球物理学报, 54(2):611-619. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201102042.htm 杜民, 胡小强, 王改云, 2014a.北黄海盆地东部坳陷东南部层序地层特征及沉积体系.海洋地质前沿, 30(1):25-33. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDT201401004.htm 杜民, 王改云, 刘金萍, 等, 2014b.北黄海盆地东部坳陷地层划分及沉积特征.特种油气藏, 21(2):51-56. http://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ201402011.htm 高顺莉, 周祖翼, 王嘹亮, 2014.北黄海侏罗系碎屑锆石U-Pb定年及地质意义.同济大学学报(自然科学版), 42(3):480-487. http://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ201403024.htm 何将启, 梁世友, 赵永强, 等, 2007.北黄海盆地地质构造特征及其在油气勘探中的意义.海洋地质与第四纪地质, 27(2):101-105. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200702017.htm 胡小强, 刘振湖, 陈玲, 等, 2009.北黄海盆地某研究区块钻井层序地层及沉积特征.海洋地质与第四纪地质, 29(2):103-110. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200902018.htm 李汉瑜, 1983.关于石英的阴极发光特征及其在砂岩研究中的应用.沉积学报, 1(2):166-171. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198302013.htm 李乐, 姚光庆, 刘永河, 等, 2015.塘沽地区沙河街组下部含云质泥岩主微量元素地球化学特征及地质意义.地球科学, 40(9):1480-1496. http://earth-science.net/WebPage/Article.aspx?id=3152 李思田, 潘元林, 陆永潮, 等, 2002.断陷湖盆隐蔽油藏预测及勘探的关键技术-高精度地震探测基础上的层序地层学研究.地球科学, 27(5):592-598. http://earth-science.net/WebPage/Article.aspx?id=1170 李三忠, 余珊, 赵淑娟, 等, 2013.东亚大陆边缘的板块重建于构造转换.海洋地质与第四纪地质, 33(3):65-94. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201303011.htm 李文勇, 李东旭, 夏斌, 等, 2006.北黄海盆地构造演化特征分析.现代地质, 20(2):268-276. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200602010.htm 李文勇, 曾祥辉, 王信国, 等, 2009.北黄海盆地构造运动学解析.地学前缘, 16(4):74-86. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200904010.htm 林畅松, 2006.沉积盆地的构造地层分析——以中国构造活动盆地研究为例.现代地质, 20(2):185-194. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200602000.htm 刘金萍, 王改云, 杜民, 等, 2013.北黄海盆地东部坳陷中生界烃源岩特征.中国海上油气, 25(4):12-16. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD201304003.htm 刘振湖, 高红芳, 胡小强, 等, 2007.北黄海盆地东部坳陷中生界含油气系统研究.中国海上油气, 19(4):229-233. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200704002.htm 刘振湖, 王飞宇, 刘金萍, 等, 2014.北黄海盆地东部坳陷油气成藏时间研究.石油实验地质, 36(5):550-554. http://www.cnki.com.cn/Article/CJFDTOTAL-SYSD201405007.htm 刘子亭, 余俊清, 张保华, 等.2006.烧失量分析在湖泊沉积与环境变化研究中的应用.盐湖研究, 14(2):67-72. http://www.cnki.com.cn/Article/CJFDTOTAL-YHYJ200602013.htm 马文涛, 於文辉, 张世晖, 2005.北黄海盆地地质构造特征及其演化.海洋地质动态, 21(11):21-27. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDT200511005.htm 田振兴, 张训华, 薛荣俊, 2004.北黄海盆地区域地质特征.海洋地质动态, 20(2):8-10, 50. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDT200402003.htm 王后金, 王嘹亮, 冯长茂, 2014.北黄海盆地的成盆动力学机制探讨.石油天然气学报, 36(5):1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201405001.htm 王嘹亮, 沈艳杰, 程日辉, 等, 2013.北黄海盆地中-上侏罗统火山岩岩石地球化学特征及构造背景.中南大学学报(自然科学版), 44(1):223-232. http://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD201301031.htm 王嘹亮, 许中杰, 程日辉, 等, 2015.北黄海盆地上侏罗统-下白垩统火山岩形成时代:锆石LA-ICP-MS U-Pb定年证据.大地构造与成矿学, 39(1):179-186. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dgyk201501016&dbname=CJFD&dbcode=CJFQ 吴淑玉, 刘俊, 2015.北黄海东部坳陷始新统米兰科维奇旋回特征.地球科学, 40(11):1933-1944. http://earth-science.net/WebPage/Article.aspx?id=3200 袁书坤, 王英民, 刘振湖, 等, 2010.北黄海盆地东部坳陷不整合类型及油气成藏模式.石油勘探与开发, 37(6):663-667. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201006005.htm 张莉, 周永章, 王嘹亮, 等, 2009.北黄海盆地生烃条件研究.天然气工业, 29(1):21-25, 131-132. http://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200901008.htm 张岳桥, 李金良, 张田, 等, 2008.胶莱盆地及其邻区白垩纪-古新世沉积构造演化历史及其区域动力学意义.地质学报, 82(9):1229-1257. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200809007.htm 郑求根, 蔡立国, 丁文龙, 等, 2005.黄海海域盆地的形成与演化.石油与天然气地质, 26(5):647-654. http://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200505016.htm -
点击查看大图
图(10) / 表(4)
计量
- 文章访问数: 5729
- HTML全文浏览量: 2565
- PDF下载量: 27
- 被引次数: 0
