[1] 贾承造,郑民,张永峰.中国非常规油气资源与勘探开发前景[J].石油勘探与开发,2012,39(2):129-135. Jia Chengzao,Zheng Min,Zhang Yongfeng.Unconventional hydrocarbon resources in China and the prospect of exploration and development[J].Petroleum Exploration and Development,2012,39(2):129-135. [2] 王永诗,巩建强,房建军,等.渤南洼陷页岩油气富集高产条件及勘探方向[J].油气地质与采收率,2012,19(6):6-10. Wang Yongshi,Gong Jianqiang,Fang Jianjun,et al.Enrichment conditions and exploration direction of shale oil in Bonan Sag[J].Petroleum Geology and Recovery Efficiency,2012,19(6):6-10. [3] 邓美寅,梁超.渤南洼陷沙三下亚段泥页岩储集空间研究:以罗69井为例[J].地学前缘,2012,19(1):173-181. Deng Meiyin,Liang Chao.Studies on reservoir space of mudstone and shale of the lower section of Es3 in Bonan Subsag:An example from Well Luo69[J].Earth Science Frontiers,2012,19(1):173-181. [4] 彭丽.陆永潮,彭鹏,等.渤海湾盆地渤南洼陷沙三下亚段泥页岩非均质性特征及演化模式——以罗69井为例[J].石油与天然气地质,2017,38(2):219-229. Peng Li,Lu Yongchao,Peng Peng,et al.Heterogeneity and evolution model of the Lower Shahejie Member 3 mud-shale in the Bonan Subsag,Bohai Bay Basin:An example from Well Luo 69[J].Oil and Gas Geology,2017,38(2):219-229. [5] Pancost R D,Freeman K H,Patzkowsky M E.Organic-matter source variation and the expression of a late Middle Ordovician carbon isotope excursion[J].Geology,1999,27(11):1015-1018. [6] Struck U,Emeis K C,Voß M,et al.Biological productivity during sapropel S5 formation in the Eastern Mediterranean Sea:Evidence from stable isotopes of nitrogen and carbon[J].Geochimica Et Cosmochimica Acta,2001,65(19):3249-3266. [7] Passier H F,Bosch H J,Nijenhuis I A,et al.Sulphidic Mediterranean surface waters during Pliocene sapropel formation[J].Nature,1999,397(6715):146-149. [8] 王鸿升,胡天跃.渤海湾盆地沾化凹陷页岩油形成影响因素分析[J].天然气地球科学,2014(增1):141-149. Wang Hongsheng,Hu Tianyue.Analysis of influence factors of shale oil formation in Zhanhua Depression of Bohai Bay Basin[J].Natural Gas Geoscience,2014,25(s1):141-149. [9] Rhodes T E,Gasse F,Lin R,et al.A Late Pleistocene-Holocene lacustrine record from Lake Manas,Zunggar (northern Xinjiang,western China)[J].Palaeogeography Palaeoclimatology Palaeoecology,1996,120(1-2):105-121. [10] Talbot M R,Livingstone D A.Hydrogen index and carbon isotopes of lacustrine organic matter as lake level indicators[J].Palaeogeography Palaeoclimatology Palaeoecology,1989,70(1):121-137. [11] Schroeder P A,Mclain A A.Illite-smectites and the influence of burial diagenesis on the geochemical cycling of nitrogen[J].Clay Minerals,1998,33(4):539-546. [12] Itihara Y,Honma H.Ammonium in biotite from metamorphic and granitic rocks of Japan[J].Geochimica Et Cosmochimica Acta,1979,43(4):503-509. [13] Thomazo C,Ader M,Philippot P.Extreme 15N-enrichments in 2.72-Gyr-old sediments:Evidence for a turning point in the nitrogen cycle[J].Geobiology,2011,9(2):107. [14] Mariotti A,Germon J C,Hubert P,et al.Experimental determination of nitrogen kinetic isotope fractionation:Some principles;illustration for the denitrification and nitrification processes[J].Plant and Soil,1981,62(3):413-430. [15] Thomazo C,Papineau D.Biogeochemical cycling of nitrogen on the early earth[J].Elements,2013,9(5):345-351. [16] Stüeken E E,Kipp M A,Koehler M C,et al.The evolution of Earth's biogeochemical nitrogen cycle[J].Earth-Science Reviews,2016,160:220-239. [17] Ader M,Thomazo C,Sansjofre P,et al.Interpretation of the nitrogen isotopic composition of Precambrian sedimentary rocks:Assumptions and perspectives[J].Chemical Geology,2016,429:93-110. [18] Laws E A,Popp B N,Bidigare R R,et al.Dependence of phytoplankton carbon isotopic composition on growth rate and[CO2)aq:Theoretical considerations and experimental results[J].Geochimica Et Cosmochimica Acta,1995,59(6):1131-1138. [19] Rau G H,Riebesell U,Wolfgladrow D.A model of photosynthetic 13C fractionation by marine phytoplankton based on diffusive molecular CO2 uptake[J].Marine Ecology Progress,1996,133(1-3):275-285. [20] Boutton T W,Archer S R,Midwood A J,et al.δ13C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem[J].Geoderma,1998,82(1-3):5-41. [21] Mampuku M,Yamanaka T,Uchida M,et al.Changes in C3/C4 vegetation in the continental interior of the Central Himalayas associated with monsoonal paleoclimatic changes during the last 600 kyr[J].Climate of the Past Discussions,2008,10(2):227-232. [22] Chow T J,Goldberg E D.On the marine geochemistry of barium[J].Geochimica Et Cosmochimica Acta,1960,20(3):192-198. [23] Bishop J K B.The barite-opal-organic carbon association in oceanic particulate matter[J].Nature,1988,332(6162):341-343. [24] Dehairs F,Chesselet R,Jedwab J.Discrete suspended particles of barite and the barium cycle in the open ocean[J].Earth and Planetary Science Letters,1980,49(2):528-550. |