东菲律宾海沉积物的磁性特征研究
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摘要
本论文旨在分析东菲律宾海帕里西维拉海盆柱样沉积物的磁性特征,以磁学参数的测量为手段,了解沉积物中所含磁性矿物的种类和含量,并分析其成因和意义,探讨研究区沉积物磁性矿物的来源,以及其所反映的古环境和古气候的演变,提供环境磁学方面的证据。
对研究区内七个柱样进行了古地磁测试,通过系统的交变退磁,得到特征磁磁倾角,据此进行磁极性期和事件划分,通过与标准极性年表比对,发现大多数柱样有清晰的高斯正极性期/松山反极性期界限,能显示到松山反极性期,并可识别出哈拉米洛正极性事件,大体判定柱样沉积物底界的年龄。根据岩芯极性带界线产出深度,参照极性年代表推算了柱样沉积物的平均沉积速率。
柱样磁化率值不高,随深度变化的曲线表现出一定的韵律性,相邻柱样的曲线特征也具有相似性。对帕里西维拉海盆西侧F090102柱样进行了系统的岩石磁学研究,测量了天然剩磁倾角、磁化率、等温剩磁、非磁滞剩磁、饱和等温剩磁等磁学参数,并进行了热磁分析。识别出松山反极性期内的哈拉米洛和奥都威正极性事件。对磁学参数及其有关比值的研究发现,岩芯磁性矿物以低矫顽力磁铁矿为主,含有少量高矫顽力磁性矿物。热磁分析发现,柱样顶段和底段沉积物除了主要的磁铁矿,可能含有一定量的钛磁铁矿,而中间部分冷却曲线位于加热曲线下方,居里点在550℃左右,可能是钛铁矿,并含有较多的富铁相钛赤铁矿。柱样沉积物中磁性矿物主要是陆源碎屑成因,岩芯底段受到海底火山作用的影响。根据磁学参数随深度的变化将岩芯分为三段,反映出沉积环境和古气候的变化。
This paper presents the results of systemic paleomagnetism investigation anddetailed rock magnetic investigation of the marine sediments from the East PhilippineSea on the basis of the application of the newly developed environmental magnetictechniques. The research of multiple magnetic parameters shows the sorts and contentof magnetic minerals in sediments. The source of magnetic mineral, the paleoclimaticvariation and sedimentary environmental changes were discussed, and theenvironmental magnetic evidence was provided.
A systemic alternating field demagnetization has been done on the seven cores.We have got the characteristic remnant magnetism of all the samples. A comparisionof geomagnetic polarity of marine sediments with the geomagnetic polarity time-scaleby A.Cox has been made, we discovered the clear boundary between Bruhnes normalepoch and Matuyama reversed epoch in most cores, the Jaramillo event during theMatuyama period was identified. The age and rate of accumulation of the sedimentshave been estimated.
The susceptibility value of marine sediments is relatively low and its curvefluctuates rhythmically. A detailed magnetic analysis has been done on the coreF090102 from the Parece Vela Basin, the following magnetic parameters weremeasured: susceptibility (χ), anhysteretic remnant magnetization (ARM), isothermalremnant magnetization (IRM), saturation isothermal remnant magnetization (SIRM),IRM-300mT (induced in a field of -300mT) and typical temperature dependence ofmagnetic susceptibility curves (χ-T). First, a magnetostratigraphic record wasobtained. The Bruhnes-Matuyama reversal, the Jaramillo event, as well as the Olduvaievent during the Matuyama period, were identified. Analyses of magnetic parameters
demonstrated that magnetic minerals in the sequence were dominated bylow-coercivity ferromagnetic minerals with subordinate high-coercivityantiferromagnetic minerals. The χ-T curves results indicate that the magneticmineralogy of the upside and bottom of the core is dominated by magnetite, maybesome titanomagnetites are included, but for the middle parts of core sediments, thecooling curves are under the heating curves, the Curie temperature is about 550℃,maybe ilmenite and some iron-enriched titanohaematite are included. The resultsshow that the rock-magnetic parameters well correspond to the paleoclimaticvariations and sedimentary environmental changes.
对研究区内七个柱样进行了古地磁测试,通过系统的交变退磁,得到特征磁磁倾角,据此进行磁极性期和事件划分,通过与标准极性年表比对,发现大多数柱样有清晰的高斯正极性期/松山反极性期界限,能显示到松山反极性期,并可识别出哈拉米洛正极性事件,大体判定柱样沉积物底界的年龄。根据岩芯极性带界线产出深度,参照极性年代表推算了柱样沉积物的平均沉积速率。
柱样磁化率值不高,随深度变化的曲线表现出一定的韵律性,相邻柱样的曲线特征也具有相似性。对帕里西维拉海盆西侧F090102柱样进行了系统的岩石磁学研究,测量了天然剩磁倾角、磁化率、等温剩磁、非磁滞剩磁、饱和等温剩磁等磁学参数,并进行了热磁分析。识别出松山反极性期内的哈拉米洛和奥都威正极性事件。对磁学参数及其有关比值的研究发现,岩芯磁性矿物以低矫顽力磁铁矿为主,含有少量高矫顽力磁性矿物。热磁分析发现,柱样顶段和底段沉积物除了主要的磁铁矿,可能含有一定量的钛磁铁矿,而中间部分冷却曲线位于加热曲线下方,居里点在550℃左右,可能是钛铁矿,并含有较多的富铁相钛赤铁矿。柱样沉积物中磁性矿物主要是陆源碎屑成因,岩芯底段受到海底火山作用的影响。根据磁学参数随深度的变化将岩芯分为三段,反映出沉积环境和古气候的变化。
This paper presents the results of systemic paleomagnetism investigation anddetailed rock magnetic investigation of the marine sediments from the East PhilippineSea on the basis of the application of the newly developed environmental magnetictechniques. The research of multiple magnetic parameters shows the sorts and contentof magnetic minerals in sediments. The source of magnetic mineral, the paleoclimaticvariation and sedimentary environmental changes were discussed, and theenvironmental magnetic evidence was provided.
A systemic alternating field demagnetization has been done on the seven cores.We have got the characteristic remnant magnetism of all the samples. A comparisionof geomagnetic polarity of marine sediments with the geomagnetic polarity time-scaleby A.Cox has been made, we discovered the clear boundary between Bruhnes normalepoch and Matuyama reversed epoch in most cores, the Jaramillo event during theMatuyama period was identified. The age and rate of accumulation of the sedimentshave been estimated.
The susceptibility value of marine sediments is relatively low and its curvefluctuates rhythmically. A detailed magnetic analysis has been done on the coreF090102 from the Parece Vela Basin, the following magnetic parameters weremeasured: susceptibility (χ), anhysteretic remnant magnetization (ARM), isothermalremnant magnetization (IRM), saturation isothermal remnant magnetization (SIRM),IRM-300mT (induced in a field of -300mT) and typical temperature dependence ofmagnetic susceptibility curves (χ-T). First, a magnetostratigraphic record wasobtained. The Bruhnes-Matuyama reversal, the Jaramillo event, as well as the Olduvaievent during the Matuyama period, were identified. Analyses of magnetic parameters
demonstrated that magnetic minerals in the sequence were dominated bylow-coercivity ferromagnetic minerals with subordinate high-coercivityantiferromagnetic minerals. The χ-T curves results indicate that the magneticmineralogy of the upside and bottom of the core is dominated by magnetite, maybesome titanomagnetites are included, but for the middle parts of core sediments, thecooling curves are under the heating curves, the Curie temperature is about 550℃,maybe ilmenite and some iron-enriched titanohaematite are included. The resultsshow that the rock-magnetic parameters well correspond to the paleoclimaticvariations and sedimentary environmental changes.
引文
1. Thompson , R., Oldfield , F., Environmental Magnetism. 1986, London: Allen & Unwin. p.141-152
2. Verosub K L., R.A.P., Environmental magnetism:past, present, and future. Journal of Geophysical Research, 1995. 100(B2): p. 2175-2192.
3. Dekkers, M.J., Environmental magnetism: an introduction. Geologie en Mijinbouw, 1997. 76: p. 163-182.
4. 刘皇风, 环境磁学. 地球科学进展, 1993. 8(2): p. 85-87.
5. 姜月华,殷鸿福,王润华, 环境磁学理论、方法和研究进展. 地球学报, 2004. 25(3): p. 357-362.
6. 张卫国,俞立中,许羽, 环境磁学研究的简介. 地球物理学进展, 1995. 10(3): p. 95-105.
7. 候红明, 环境磁学的进展与展望. 南海研究与开发, 1996(4): p. 36-42.
8. 邓成龙,袁宝印,胡守云,刘东生等, 环境磁学某些研究进展述评. 海洋地质与第四纪地质, 2000. 20(2): p. 93-101.
9. 刘椿, 古地磁学导论. 1 ed. 1991, 北京: 科学出版社.
10. 朱日祥,岳乐平,白立新, 中国第四纪古地磁学研究进展. 第四纪研究, 1995(2): p. 162-173.
11. Yu Lizhong et al., Palaeoenvironmental implications of magnetic measurements on sediment core form Kunming Basin Southwest China. Journal of Paleolimnology, 1990(3): p. 95-111.
12. 张树夫,肖家仪,俞立中,吴玉书, 沉积物矿物磁性测量在古环境研究中的应用. 地理科学, 1991. 11(2): p. 182-195.
13. 张普纲,樊行昭,霍俊杰, 磁性参数的环境指示意义. 太原理工大学学报, 2003. 34(3): p. 301-305.
14. 蓝先洪, Heinrich 事件的全球性意义. 海洋地质动态, 2000. 16(8): p. 5-8.
15. 任剑璋,刘东生,周晓权等, 气候不稳定性记录研究的新进展. 海洋地质与第四纪地质, 1998. 18(2): p. 49-58.
16. 张世红,李海燕, 地磁学、古地磁学和环境磁学的研究新进展———第 32届国际地质大会学科总结和评述. 现代地质, 2004. 18(4): p. 415-423.
17. Walden, J., Environmental magnetism: principles and applications of enviromagnetics. Quaternary Science Reviews, 2004(23): p. 1867-1870.
18. Oldfield.F., Environmental magnetism-A personal perspective. Quaternary Science Reviews, 1991. 10: p. 73-85.
19. Robinson, S.G., The late Pleistocene paleoclimate record of North Atlantic deep-sea sediments revealed by mineral magnetic measurements. Phys. Earth Planet. Inter., 1986. 42: p. 22-47.
20. Eva Moreno, N.T., Doriane Delanghe, I. Nick McCave, Nick J. Shackleton, Climatic and oceanographic changes in the Northeast Atlantic reflected by magnetic properties of sediments deposited on the Portuguese Margin during the last 340 ka. Earth and Planetary Science Letters, 2002. 202: p. 465-480.
21. C. Kissel , C.L., et al., Rapid climatic variations during marine isotopic stage 3: magnetic analysis of sediments from Nordic Seas and North Atlantic. Earth and Planetary Science Letters, 1999(171): p. 489-502.
22. 吴瑞金, 湖泊沉积物的磁化率、频率磁化率及其古气候意义--以青海湖、岱海近代沉积为例. 湖泊科学, 1993. 5(2): p. 128-135.
23. 吴能友,段威武,刘坚, 南极布兰斯菲尔德海峡晚第四纪沉积物磁组构特征及其古环境学意义. 海洋地质与第四纪地质, 1998. 18(1): p. 77-88.
24. 丛友滋、韩国忠、李从先等, 泥质潮坪磁组构特征及其意义研究. 海洋地质与第四纪地质, 1997. 17(2): p. 13-16.
25. 胡蒙育,B.Maher, 中国黄土堆积的磁性记录与古降雨量重建. 地球科学进展, 2002. 17(3): p. 20-26.
26. Mather B A, T.R., Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols. Quaternary Science Research, 1992. 37: p. 155-170.
27. 贾玉连、柯贤坤、王艳等, 渤海曹妃甸沙坝-泻湖海岸现代沉积的磁化率与粒度、矿物的关系. 海洋通报, 2000. 19(1): p. 41-50.
28. 候红明,王保贵,汤贤赞, 南极普里兹湾 NP93-2 柱样磁组构特征及其古气候意义. 地球物理学报, 1996. 30(5): p. 625-630.
29. 潘永信,朱日祥, 磁组构研究现状. 地球物理学进展, 1998. 13(1): p. 52-59.
30. C. Kissel , C.L., A. Mazaud , T. Dokken, Magnetic anisotropy and environmental changes in two sedimentary cores from the Norwegian Sea and the North Atlantic. Earth and Planetary Science Letters, 1998(164): p. 617-626.
31. 王俊达, 第四纪沉积物的古地磁研究. 第四纪研究, 1992(1): p. 39-44.
32. 汤贤赞,陈木宏,颜文,陈忠, 西太平洋暖池两柱样沉积物的磁性地层学研究. 热带海洋, 1999. 18(4): p. 1-7.
33. 汤贤赞,陈忠,颜文,陈木宏, 西太平洋暖池温区中心沉积物磁化率记录的 YD 和 Heinrich 冷事件. 科学通报, 2003. 48(5): p. 491-496.
34. A. Mazaud , M.A.S., et al, Geomagnetic-assisted stratigraphy and sea surface temperature changes in core MD94-103 (Southern Indian Ocean): possible implications for North^South climatic relationships around H4. Earth and Planetary Science Letters, 2002(201): p. 159-170.
35. Catherine Kissel , C.L., Steven Clemens , Peter Solheid, Magnetic signature of environmental changes in the last 1.2 Myr at ODP Site 1146, South China Sea. Marine Geology, 2003(201): p. 119-132.
36. 汤贤赞,王保贵,袁友仁等, 南沙海区沉积物剩余磁化强度与古气候旋回. 热带海洋, 1993. 12(3): p. 32-37.
37. 候红明,汤贤赞,王保贵, 南沙海域沉积物古地磁学参数对米兰科维奇周期的响应. 热带海洋, 1995. 14(3): p. 1-7.
38. 候红明,王保贵,汤贤赞, 南海北部沉积物磁化率对古气候非线性变化的响应. 热带海洋, 1996. 15(3): p. 1-5.
39. Yamazaki T, K.I., Marumo K., Origin of stable remanent magnetization of siliceous sediments in the central equatorial Pacific. Earth and Planetary Science Letters, 1991(105): p. 81-93.
40. Karlin, R., Magnetite Diagenesis in marine sediments from the Oregon continental margin. Journal of Geophysical Research, 1990. 95(B4): p. 4405-4419.
41. 刘健, 磁性矿物还原成岩作用述评. 海洋地质与第四纪地质, 2000. 20(4): p. 103-107.
42. Hilton. J., L., J.P.and Chapman.J.S.,, Magnetic and chemical characterisation of a diagenetic magnetic formed in the sediments of productive lakes. Chemical Geology, 1986(56): p. 325-335.
43. 刘健,朱日祥,李绍全,Jeong-Hae Chang, 南黄海东南部冰后期泥质沉积物中磁性矿物的成岩变化极其对环境变化的响应. 中国科学(D 辑), 2003. 33(6): p. 583-592.
44. Simon G.Robinson , J.T.S.S., Frank Oldfield, Early diagenesis in North Atlantic abyssal plain sediments characterized by rock-magnetic and geochemical indices. Marine Geology, 2000. 163(77-107).
45. Karlin R, L.S., Geochemical and sedimentological control of the magnetic properties of hemipelagic sediments. Journal of Geophysical Research, 1985. 90(B12): p. 10373-10392.
46. Kirsehvink, J.L., Paleomagnetic cvidence for fossil biogenic magnetite in western Crete. Earth and Planetary Science Letters, 1982(59): p. 388-392.
47. Petersen, N., Dobeneck, T.and Vali, H.,, Fossil bacterial magnetite in deep-sea sediments from the South Atlantic Ocean. Nature, 1986(320): p. 611-615.
48. Ellwood, B.B., 缺氧深海沉积物中菱铁矿的形成--细菌协合过程在古地磁学中的重要意义. Geology, 1988. 16: p. 980-982.
49. M.E.Evans, H.F., Bloemendal J, Thouveny N . Natural magnetic archives of past global change. Surveys in Geophysics, 1997(18): p. 183-196.
50. Chen.X.D., W.D.F., Yuan, et al, Paleomagnetism and paleoclimate change in the South China Sea since the late Pleistocene. Acta Oceanologica Sinica, 1992. 11(4): p. 573-581.
51. 汤贤赞, 开展南海环境磁学研究的重要性. 南海研究与开发, 1997(1): p. 27-29.
52. 候红明,王保贵,汤贤赞, 南极 15ka 以来海洋沉积物的环境磁学研究. 极 地研究, 1997. 9(1): p. 35-43.
53. Liu Jian, Z.R., Li Guangxue, et al, Rock magnetic properties of the fine-grained sediment on the outer shelf of the East China Sea: implication for provenance. Marine Geology, 2003. 193: p. 195-206.
54. Liu Jian, Z.R., Andrew P. Roberts, et al, High-resolution analysis of early diagenetic effects on magnetic minerals in post-middle-Holocene continental shelf sediments from the Korea Strait. Journal of Geophysical Research, 2004. 109: p. 1-15.
55. 汤贤赞、唐诚、陈木宏等, 南沙群岛永暑礁钻井珊瑚礁和珊瑚碎屑的磁学分析. 热带海洋学报, 2003. 22(3): p. 44-52.
56. 张明书、刘健、周墨清, 西永 1 井礁序列的磁化率研究. 科学通报, 1994. 39(4): p. 340-343.
57. 李萍、李培英、张晓龙等, 冲绳海槽沉积物不同粒级的磁性特征及其与环境的关系. 科学通报, 2005. 50(3): p. 262-269.
58. 张卫国、俞立中、丛友滋, 赤道东太平洋 C-C 区硅质沉积物的磁性特征及细菌合成磁铁矿. 沉积学报, 2003. 21(3): p. 467-473.
59. Liu Zongyang, Rock magnetic study of marine sediments and its application to paleoenvironmental research. Doctoral dissertation. 1994: Kyoto University.
60. 葛淑兰,石学法,韩贻兵, 南黄海海底沉积物的磁化率特征. 科学通报, 2001. 46: p. 34-39.
61. 葛宗诗, 南黄海 QC2 孔磁化率研究. 海洋地质与第四纪地质, 1996. 16(4): p. 35-42.
62. 杨小强,李华梅,周永章, 南海南部 NS93—5 孔沉积物磁化率特征及其对全球气候变化的记录. 海洋地质与第四纪地质, 2002. 22(1): p. 31-36.
63. 张卫国、俞立中、李纬显, 东海陆架表层沉积物的磁性测量及其油气勘探意义. 华东师范大学学报(自然科学版), 1998. 1: p. 76-81.
64. 陈满荣、俞立中、韩晓非, 环境磁学样品干燥过程中的磁性效应. 沉积学报, 2001. 19(4): p. 30-37.
65. 王建,刘泽纯,姜文英,董龄祥,朱明哲,高丰, 磁化率与粒度、矿物的 关系及其古环境意义. 地理学报, 1996. 51(2): p. 155-163.
66. 王恩德、王丹丽、王毅, 铁矿物形成过程中的细菌作用研究. 岩石矿物学杂志, 2001. 20(4): p. 14-19.
67. Michael E.Evans, F.H., Environmental Magnetism -Principles and Applications of Enviromagnetics. 2003, New York: Academic Press.
68. 刘健, 黄东海及朝鲜海峡冰后期陆架沉积物的环境磁学研究. 博士论文, 2003: p. 3-18.
69. 李常珍、李乃胜、林美华, 菲律宾海的地势特征. 海洋科学, 2000. 24(6): p. 47-52.
70. (苏)A.B.佩纬主编,刘昭蜀、于珏译, 菲律宾海地质. 1989, 北京: 海洋出版社. 1-250.
71. 任建业,李思田, 西太平洋边缘海盆地的扩张过程和动力学背景. 地学前缘, 2000. 7(3): p. 203-213.
72. 金性春, 大洋钻探与西太平洋构造. 地球科学进展, 1995. 10(3): p. 234-239.
73. 辛春译, 菲律宾海海底的构造单元(沿北纬 18°地学断面). 太平洋地质学, 1989. 6: p. 1-10.
74. Karig, D.E., Basin Genesis In The Philippine Sea. Initial reports of the deep sea drilling projects[POD], 1981. Leg 31: p. 857-878.
75. Cary L.Mrozowski, D.E.H., The evolution of the Parece Vela Basin, eastern Philippine Sea. Earth and Planetary Science Letters, 1979. 46(1): p. 49-67.
76. V.P.Nechaev,金康辰译, 据碎屑沉积物记录的菲律宾海和日本海的演化. Marine Geology, 1991. 97: p. 167-190.
77. 张弦,俞慕耕,江伟等, 菲律宾海及其邻近海区的水文特征. 海洋通报, 2004. 23(1): p. 8-14.
78. 张弦,俞慕耕,江伟,李培, 菲律宾海及其邻近海区的水文特征. 海洋通报, 2004. 23(1): p. 8-14.
79. 王凡,张平城,胡敦欣,H.Seidle, 热带西太平洋环流及其季节变化. 科学通报, 2001. 46(23): p. 1998.
80. 闾国年, 距今三万年来西北太平洋洋流系统变化的初步研究. 海洋科学, 1989(3): p. 13-20.
81. 李丽娟,刘秦玉,刘伟, 太平洋北赤道流表层流速及分叉点位置. 中国海洋大学学报, 2005. 35(3): p. 370-374.
82. 孙湘平, 西北太平洋副热带逆流、北赤道流、北赤道逆流几个特征的比较. 黄渤海海洋, 2000. 18(1): p. 1-12.
83. 孙守勋,滕军, 菲律宾海的气候特征. 海洋预报, 2003. 20(3): p. 31-39.
84. 葛淑兰、石学法、朱日祥等, 南黄海 EY02-2 孔磁性地层及古环境意义. 科学通报, 2005. 50(22): p. 2531-2541.
85. D.W.Collinson, Methods in Rock Magnetism and Palaomagnetism Technigues and Instrumentation. 1983, London New York: Chapman and Hall.
86. 魏青云, 推进古地磁研究的着力点. 学科发展与研究, 1990. 5: p. 35-40.
87. J.Hilton.张志良译, 解释湖成和海成沉积物磁性记录的一种简单模式. Quaternary Research, 1987. 27: p. 160-166.
88. 王永红、沈焕庭、张卫国, 长江与黄河河口沉积物磁性特征对比的初步研究. 沉积学报, 2004. 22(4): p. 658-664.
89. M.A.Williams, D.L.D., P.De Deckker, A.P.Kershaw, T.J.Stokes, Quaternary Environments. 1993: Edward Arnold Ltd.
90. 朱立平、陈玲、陈平中等, 环境磁学反映的藏南沉错地区 1300 年来冷暖变化. 第四纪研究, 2001. 21(6): p. 520-527.
91. 俞立中、许羽、许世远等, 太湖沉积物的磁性特征及其环境意义. 湖泊科学, 1995. 7(2): p. 141-150.
92. 俞立中、许羽、张卫国, 湖泊沉积物的矿物磁性测量及其环境应用. 地球物理学进展, 1995. 10(1): p. 11-22.
93. Maher, B.A., Charcterisation of soils mineral magnetic measurements. Phys. Earth Planet. Inter., 1985. 42: p. 76-92.
94. 曹希强、郑祥民、周立旻等, 洪湖沉积物的磁性特征及其环境意义. 湖泊科学, 2004. 16(3): p. 227-232.
95. 贾海林,刘苍宇,张卫国, 崇明岛 CY 孔沉积物的磁性特征及其环境意义. 沉积学报, 2004. 22(1): p. 117-124.
96. Thompson, R., Modelling magnetization data using SP. Physics of the Earth and Planetary, 1986. 42: p. 113-127.
97. Thompson R, B.J., Dearing J A, Oldfield F, Rummery T A, Stober J C,Turner G M., Environmental applications of magnetic measurements. Science, 1980. 207: p. 481~486.
98. Roberts A P, T.G.M., Diagenetic formation of ferromagnetic iron sulphide minerals in rapidly deposited marine sediments, South Island, New Zealand. Earth and Planetary Science Letters, 1993. 115: p. 257-273.
99. Doris M Curtis, e.a., Lithofacies of the Shikoku basin and the Parace Vela basin. Initial reports of the deep sea drilling projects[POD], 1980(58): p. 701-709.
100. 许淑梅、张晓东、翟世奎, 四国海盆起源与沉积环境演化. 海洋地质与第四纪地质, 2004. 24(2): p. 119-124.
101. 陈萍、何报寅、杜耘, 1200a 来洪湖演变的环境磁学记录. 沉积学报, 2005. 23(1): p. 138-143.
102. 王律江, 上新世末～更新世初西太平洋变冷事件及其古气候意义. 第四纪研究, 1996(4): p. 300-309.
103. 李华梅, 地磁场倒转和古地磁年表. 地质地球化学, 1974. 12: p. 1-7.
104. 苏朴、刘椿, 布莱克(Blake)负向极性幕研究的新进展. 地球物理学进展, 1995. 10(2): p. 99-106.
105. 赵松龄、张宏才, 晚更新世末期的地磁短期反极性事件. 海洋地质研究, 1981. 1(2): p. 61-68.
106. 孙维敏、张宏才、李本兆, 东海 DC-1,DC-2 孔古地磁研究. 海洋科学, 1989(5): p. 15-24.
107. Harland, W.B., Cox,A.V.,et al., A geologic time scale. 1982: Cambridge Earth science series, Cambridge University Press.
108. Loren Kroenke, R.S., et al., West side of the Parece Vela Basin, in Initial Reports of the Deep Sea Drilling Projects, Volume LIX. 1981. p. 320-335.
109. 周墨清, 太平洋中部磁性地层学研究. 海洋地质与第四纪地质, 1995. 15(1): p. 41-56.
110. Mull R, M.D., Geomagnetic reversals. Geotimes, 1989. 20( 20).
111. 丛友滋、李素玲、程国良等, 黄海两钻孔岩芯的古地磁分析. 地震地质, 1980. 2(3): p. 64-69.
112. 小山真人,沈耀龙译, 据古地磁资料探讨菲律宾海板块构造发育史. 地学杂志, 1991. 4.
113. 李粹中, 南海深海短柱样的磁性地层学特征. 沉积学报, 1994. 12(3): p. 136-142.
114. Horng C S, R.A.P., Liang W T., A 2.14Myr astronomically tuned record of relative geomagnetic paleointensity from the western Pillippine Sea. Journal of Geophysical Research, 2003. 108(B1): p. 1-15.
115. 季军良、郑洪波、刘锐等, 邙山黄土地层再研究. 海洋地质与第四纪地质, 2004. 24(4): p. 101-109.
116. Reynolds R L, K.J.W., Magnetic records of climate change. Rev.Geophys,Supplement, 1995: p. 101-110.
117. 鹿化煜、安芷生, 洛川黄土粒度组成的古气候意义. 科学通报, 1997. 42(1): p. 66-69.
118. 李军、高抒、孙有斌等, 冲绳海槽南部沉积层序的粒度特征. 沉积学报, 2003. 21(3): p. 461-467.
119. 杨小强、李华梅, 泥河湾盆地沉积物粒度组分与磁化率变化相关性研究. 沉积学报, 2002. 20(4): p. 675-680.
120. 杨小强、李华梅, 泥河湾盆地沉积物磁化率及粒度参数对沉积环境的响应. 沉积学报, 1999. 17(增刊): p. 763-769.
121. Taylor RM, M.B., Self PG, Magnetite in soils: the synthesis of single-Domain and superparamagnetic magnetite. Clay Minerals, 1987. 22: p. 411-422.
122. 韩晓非、张卫国、陈满荣等, 长江口潮滩植物对沉积物铁的地球化学循环及磁性特征的影响. 沉积学报, 2003. 21(3): p. 495-500.
123. 张卫国、俞立中、陆敏, 长江口潮滩沉积物氧化铁与磁性特征的关系. 地
球物理学报, 2003. 46(1): p. 79-86.
2. Verosub K L., R.A.P., Environmental magnetism:past, present, and future. Journal of Geophysical Research, 1995. 100(B2): p. 2175-2192.
3. Dekkers, M.J., Environmental magnetism: an introduction. Geologie en Mijinbouw, 1997. 76: p. 163-182.
4. 刘皇风, 环境磁学. 地球科学进展, 1993. 8(2): p. 85-87.
5. 姜月华,殷鸿福,王润华, 环境磁学理论、方法和研究进展. 地球学报, 2004. 25(3): p. 357-362.
6. 张卫国,俞立中,许羽, 环境磁学研究的简介. 地球物理学进展, 1995. 10(3): p. 95-105.
7. 候红明, 环境磁学的进展与展望. 南海研究与开发, 1996(4): p. 36-42.
8. 邓成龙,袁宝印,胡守云,刘东生等, 环境磁学某些研究进展述评. 海洋地质与第四纪地质, 2000. 20(2): p. 93-101.
9. 刘椿, 古地磁学导论. 1 ed. 1991, 北京: 科学出版社.
10. 朱日祥,岳乐平,白立新, 中国第四纪古地磁学研究进展. 第四纪研究, 1995(2): p. 162-173.
11. Yu Lizhong et al., Palaeoenvironmental implications of magnetic measurements on sediment core form Kunming Basin Southwest China. Journal of Paleolimnology, 1990(3): p. 95-111.
12. 张树夫,肖家仪,俞立中,吴玉书, 沉积物矿物磁性测量在古环境研究中的应用. 地理科学, 1991. 11(2): p. 182-195.
13. 张普纲,樊行昭,霍俊杰, 磁性参数的环境指示意义. 太原理工大学学报, 2003. 34(3): p. 301-305.
14. 蓝先洪, Heinrich 事件的全球性意义. 海洋地质动态, 2000. 16(8): p. 5-8.
15. 任剑璋,刘东生,周晓权等, 气候不稳定性记录研究的新进展. 海洋地质与第四纪地质, 1998. 18(2): p. 49-58.
16. 张世红,李海燕, 地磁学、古地磁学和环境磁学的研究新进展———第 32届国际地质大会学科总结和评述. 现代地质, 2004. 18(4): p. 415-423.
17. Walden, J., Environmental magnetism: principles and applications of enviromagnetics. Quaternary Science Reviews, 2004(23): p. 1867-1870.
18. Oldfield.F., Environmental magnetism-A personal perspective. Quaternary Science Reviews, 1991. 10: p. 73-85.
19. Robinson, S.G., The late Pleistocene paleoclimate record of North Atlantic deep-sea sediments revealed by mineral magnetic measurements. Phys. Earth Planet. Inter., 1986. 42: p. 22-47.
20. Eva Moreno, N.T., Doriane Delanghe, I. Nick McCave, Nick J. Shackleton, Climatic and oceanographic changes in the Northeast Atlantic reflected by magnetic properties of sediments deposited on the Portuguese Margin during the last 340 ka. Earth and Planetary Science Letters, 2002. 202: p. 465-480.
21. C. Kissel , C.L., et al., Rapid climatic variations during marine isotopic stage 3: magnetic analysis of sediments from Nordic Seas and North Atlantic. Earth and Planetary Science Letters, 1999(171): p. 489-502.
22. 吴瑞金, 湖泊沉积物的磁化率、频率磁化率及其古气候意义--以青海湖、岱海近代沉积为例. 湖泊科学, 1993. 5(2): p. 128-135.
23. 吴能友,段威武,刘坚, 南极布兰斯菲尔德海峡晚第四纪沉积物磁组构特征及其古环境学意义. 海洋地质与第四纪地质, 1998. 18(1): p. 77-88.
24. 丛友滋、韩国忠、李从先等, 泥质潮坪磁组构特征及其意义研究. 海洋地质与第四纪地质, 1997. 17(2): p. 13-16.
25. 胡蒙育,B.Maher, 中国黄土堆积的磁性记录与古降雨量重建. 地球科学进展, 2002. 17(3): p. 20-26.
26. Mather B A, T.R., Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols. Quaternary Science Research, 1992. 37: p. 155-170.
27. 贾玉连、柯贤坤、王艳等, 渤海曹妃甸沙坝-泻湖海岸现代沉积的磁化率与粒度、矿物的关系. 海洋通报, 2000. 19(1): p. 41-50.
28. 候红明,王保贵,汤贤赞, 南极普里兹湾 NP93-2 柱样磁组构特征及其古气候意义. 地球物理学报, 1996. 30(5): p. 625-630.
29. 潘永信,朱日祥, 磁组构研究现状. 地球物理学进展, 1998. 13(1): p. 52-59.
30. C. Kissel , C.L., A. Mazaud , T. Dokken, Magnetic anisotropy and environmental changes in two sedimentary cores from the Norwegian Sea and the North Atlantic. Earth and Planetary Science Letters, 1998(164): p. 617-626.
31. 王俊达, 第四纪沉积物的古地磁研究. 第四纪研究, 1992(1): p. 39-44.
32. 汤贤赞,陈木宏,颜文,陈忠, 西太平洋暖池两柱样沉积物的磁性地层学研究. 热带海洋, 1999. 18(4): p. 1-7.
33. 汤贤赞,陈忠,颜文,陈木宏, 西太平洋暖池温区中心沉积物磁化率记录的 YD 和 Heinrich 冷事件. 科学通报, 2003. 48(5): p. 491-496.
34. A. Mazaud , M.A.S., et al, Geomagnetic-assisted stratigraphy and sea surface temperature changes in core MD94-103 (Southern Indian Ocean): possible implications for North^South climatic relationships around H4. Earth and Planetary Science Letters, 2002(201): p. 159-170.
35. Catherine Kissel , C.L., Steven Clemens , Peter Solheid, Magnetic signature of environmental changes in the last 1.2 Myr at ODP Site 1146, South China Sea. Marine Geology, 2003(201): p. 119-132.
36. 汤贤赞,王保贵,袁友仁等, 南沙海区沉积物剩余磁化强度与古气候旋回. 热带海洋, 1993. 12(3): p. 32-37.
37. 候红明,汤贤赞,王保贵, 南沙海域沉积物古地磁学参数对米兰科维奇周期的响应. 热带海洋, 1995. 14(3): p. 1-7.
38. 候红明,王保贵,汤贤赞, 南海北部沉积物磁化率对古气候非线性变化的响应. 热带海洋, 1996. 15(3): p. 1-5.
39. Yamazaki T, K.I., Marumo K., Origin of stable remanent magnetization of siliceous sediments in the central equatorial Pacific. Earth and Planetary Science Letters, 1991(105): p. 81-93.
40. Karlin, R., Magnetite Diagenesis in marine sediments from the Oregon continental margin. Journal of Geophysical Research, 1990. 95(B4): p. 4405-4419.
41. 刘健, 磁性矿物还原成岩作用述评. 海洋地质与第四纪地质, 2000. 20(4): p. 103-107.
42. Hilton. J., L., J.P.and Chapman.J.S.,, Magnetic and chemical characterisation of a diagenetic magnetic formed in the sediments of productive lakes. Chemical Geology, 1986(56): p. 325-335.
43. 刘健,朱日祥,李绍全,Jeong-Hae Chang, 南黄海东南部冰后期泥质沉积物中磁性矿物的成岩变化极其对环境变化的响应. 中国科学(D 辑), 2003. 33(6): p. 583-592.
44. Simon G.Robinson , J.T.S.S., Frank Oldfield, Early diagenesis in North Atlantic abyssal plain sediments characterized by rock-magnetic and geochemical indices. Marine Geology, 2000. 163(77-107).
45. Karlin R, L.S., Geochemical and sedimentological control of the magnetic properties of hemipelagic sediments. Journal of Geophysical Research, 1985. 90(B12): p. 10373-10392.
46. Kirsehvink, J.L., Paleomagnetic cvidence for fossil biogenic magnetite in western Crete. Earth and Planetary Science Letters, 1982(59): p. 388-392.
47. Petersen, N., Dobeneck, T.and Vali, H.,, Fossil bacterial magnetite in deep-sea sediments from the South Atlantic Ocean. Nature, 1986(320): p. 611-615.
48. Ellwood, B.B., 缺氧深海沉积物中菱铁矿的形成--细菌协合过程在古地磁学中的重要意义. Geology, 1988. 16: p. 980-982.
49. M.E.Evans, H.F., Bloemendal J, Thouveny N . Natural magnetic archives of past global change. Surveys in Geophysics, 1997(18): p. 183-196.
50. Chen.X.D., W.D.F., Yuan, et al, Paleomagnetism and paleoclimate change in the South China Sea since the late Pleistocene. Acta Oceanologica Sinica, 1992. 11(4): p. 573-581.
51. 汤贤赞, 开展南海环境磁学研究的重要性. 南海研究与开发, 1997(1): p. 27-29.
52. 候红明,王保贵,汤贤赞, 南极 15ka 以来海洋沉积物的环境磁学研究. 极 地研究, 1997. 9(1): p. 35-43.
53. Liu Jian, Z.R., Li Guangxue, et al, Rock magnetic properties of the fine-grained sediment on the outer shelf of the East China Sea: implication for provenance. Marine Geology, 2003. 193: p. 195-206.
54. Liu Jian, Z.R., Andrew P. Roberts, et al, High-resolution analysis of early diagenetic effects on magnetic minerals in post-middle-Holocene continental shelf sediments from the Korea Strait. Journal of Geophysical Research, 2004. 109: p. 1-15.
55. 汤贤赞、唐诚、陈木宏等, 南沙群岛永暑礁钻井珊瑚礁和珊瑚碎屑的磁学分析. 热带海洋学报, 2003. 22(3): p. 44-52.
56. 张明书、刘健、周墨清, 西永 1 井礁序列的磁化率研究. 科学通报, 1994. 39(4): p. 340-343.
57. 李萍、李培英、张晓龙等, 冲绳海槽沉积物不同粒级的磁性特征及其与环境的关系. 科学通报, 2005. 50(3): p. 262-269.
58. 张卫国、俞立中、丛友滋, 赤道东太平洋 C-C 区硅质沉积物的磁性特征及细菌合成磁铁矿. 沉积学报, 2003. 21(3): p. 467-473.
59. Liu Zongyang, Rock magnetic study of marine sediments and its application to paleoenvironmental research. Doctoral dissertation. 1994: Kyoto University.
60. 葛淑兰,石学法,韩贻兵, 南黄海海底沉积物的磁化率特征. 科学通报, 2001. 46: p. 34-39.
61. 葛宗诗, 南黄海 QC2 孔磁化率研究. 海洋地质与第四纪地质, 1996. 16(4): p. 35-42.
62. 杨小强,李华梅,周永章, 南海南部 NS93—5 孔沉积物磁化率特征及其对全球气候变化的记录. 海洋地质与第四纪地质, 2002. 22(1): p. 31-36.
63. 张卫国、俞立中、李纬显, 东海陆架表层沉积物的磁性测量及其油气勘探意义. 华东师范大学学报(自然科学版), 1998. 1: p. 76-81.
64. 陈满荣、俞立中、韩晓非, 环境磁学样品干燥过程中的磁性效应. 沉积学报, 2001. 19(4): p. 30-37.
65. 王建,刘泽纯,姜文英,董龄祥,朱明哲,高丰, 磁化率与粒度、矿物的 关系及其古环境意义. 地理学报, 1996. 51(2): p. 155-163.
66. 王恩德、王丹丽、王毅, 铁矿物形成过程中的细菌作用研究. 岩石矿物学杂志, 2001. 20(4): p. 14-19.
67. Michael E.Evans, F.H., Environmental Magnetism -Principles and Applications of Enviromagnetics. 2003, New York: Academic Press.
68. 刘健, 黄东海及朝鲜海峡冰后期陆架沉积物的环境磁学研究. 博士论文, 2003: p. 3-18.
69. 李常珍、李乃胜、林美华, 菲律宾海的地势特征. 海洋科学, 2000. 24(6): p. 47-52.
70. (苏)A.B.佩纬主编,刘昭蜀、于珏译, 菲律宾海地质. 1989, 北京: 海洋出版社. 1-250.
71. 任建业,李思田, 西太平洋边缘海盆地的扩张过程和动力学背景. 地学前缘, 2000. 7(3): p. 203-213.
72. 金性春, 大洋钻探与西太平洋构造. 地球科学进展, 1995. 10(3): p. 234-239.
73. 辛春译, 菲律宾海海底的构造单元(沿北纬 18°地学断面). 太平洋地质学, 1989. 6: p. 1-10.
74. Karig, D.E., Basin Genesis In The Philippine Sea. Initial reports of the deep sea drilling projects[POD], 1981. Leg 31: p. 857-878.
75. Cary L.Mrozowski, D.E.H., The evolution of the Parece Vela Basin, eastern Philippine Sea. Earth and Planetary Science Letters, 1979. 46(1): p. 49-67.
76. V.P.Nechaev,金康辰译, 据碎屑沉积物记录的菲律宾海和日本海的演化. Marine Geology, 1991. 97: p. 167-190.
77. 张弦,俞慕耕,江伟等, 菲律宾海及其邻近海区的水文特征. 海洋通报, 2004. 23(1): p. 8-14.
78. 张弦,俞慕耕,江伟,李培, 菲律宾海及其邻近海区的水文特征. 海洋通报, 2004. 23(1): p. 8-14.
79. 王凡,张平城,胡敦欣,H.Seidle, 热带西太平洋环流及其季节变化. 科学通报, 2001. 46(23): p. 1998.
80. 闾国年, 距今三万年来西北太平洋洋流系统变化的初步研究. 海洋科学, 1989(3): p. 13-20.
81. 李丽娟,刘秦玉,刘伟, 太平洋北赤道流表层流速及分叉点位置. 中国海洋大学学报, 2005. 35(3): p. 370-374.
82. 孙湘平, 西北太平洋副热带逆流、北赤道流、北赤道逆流几个特征的比较. 黄渤海海洋, 2000. 18(1): p. 1-12.
83. 孙守勋,滕军, 菲律宾海的气候特征. 海洋预报, 2003. 20(3): p. 31-39.
84. 葛淑兰、石学法、朱日祥等, 南黄海 EY02-2 孔磁性地层及古环境意义. 科学通报, 2005. 50(22): p. 2531-2541.
85. D.W.Collinson, Methods in Rock Magnetism and Palaomagnetism Technigues and Instrumentation. 1983, London New York: Chapman and Hall.
86. 魏青云, 推进古地磁研究的着力点. 学科发展与研究, 1990. 5: p. 35-40.
87. J.Hilton.张志良译, 解释湖成和海成沉积物磁性记录的一种简单模式. Quaternary Research, 1987. 27: p. 160-166.
88. 王永红、沈焕庭、张卫国, 长江与黄河河口沉积物磁性特征对比的初步研究. 沉积学报, 2004. 22(4): p. 658-664.
89. M.A.Williams, D.L.D., P.De Deckker, A.P.Kershaw, T.J.Stokes, Quaternary Environments. 1993: Edward Arnold Ltd.
90. 朱立平、陈玲、陈平中等, 环境磁学反映的藏南沉错地区 1300 年来冷暖变化. 第四纪研究, 2001. 21(6): p. 520-527.
91. 俞立中、许羽、许世远等, 太湖沉积物的磁性特征及其环境意义. 湖泊科学, 1995. 7(2): p. 141-150.
92. 俞立中、许羽、张卫国, 湖泊沉积物的矿物磁性测量及其环境应用. 地球物理学进展, 1995. 10(1): p. 11-22.
93. Maher, B.A., Charcterisation of soils mineral magnetic measurements. Phys. Earth Planet. Inter., 1985. 42: p. 76-92.
94. 曹希强、郑祥民、周立旻等, 洪湖沉积物的磁性特征及其环境意义. 湖泊科学, 2004. 16(3): p. 227-232.
95. 贾海林,刘苍宇,张卫国, 崇明岛 CY 孔沉积物的磁性特征及其环境意义. 沉积学报, 2004. 22(1): p. 117-124.
96. Thompson, R., Modelling magnetization data using SP. Physics of the Earth and Planetary, 1986. 42: p. 113-127.
97. Thompson R, B.J., Dearing J A, Oldfield F, Rummery T A, Stober J C,Turner G M., Environmental applications of magnetic measurements. Science, 1980. 207: p. 481~486.
98. Roberts A P, T.G.M., Diagenetic formation of ferromagnetic iron sulphide minerals in rapidly deposited marine sediments, South Island, New Zealand. Earth and Planetary Science Letters, 1993. 115: p. 257-273.
99. Doris M Curtis, e.a., Lithofacies of the Shikoku basin and the Parace Vela basin. Initial reports of the deep sea drilling projects[POD], 1980(58): p. 701-709.
100. 许淑梅、张晓东、翟世奎, 四国海盆起源与沉积环境演化. 海洋地质与第四纪地质, 2004. 24(2): p. 119-124.
101. 陈萍、何报寅、杜耘, 1200a 来洪湖演变的环境磁学记录. 沉积学报, 2005. 23(1): p. 138-143.
102. 王律江, 上新世末～更新世初西太平洋变冷事件及其古气候意义. 第四纪研究, 1996(4): p. 300-309.
103. 李华梅, 地磁场倒转和古地磁年表. 地质地球化学, 1974. 12: p. 1-7.
104. 苏朴、刘椿, 布莱克(Blake)负向极性幕研究的新进展. 地球物理学进展, 1995. 10(2): p. 99-106.
105. 赵松龄、张宏才, 晚更新世末期的地磁短期反极性事件. 海洋地质研究, 1981. 1(2): p. 61-68.
106. 孙维敏、张宏才、李本兆, 东海 DC-1,DC-2 孔古地磁研究. 海洋科学, 1989(5): p. 15-24.
107. Harland, W.B., Cox,A.V.,et al., A geologic time scale. 1982: Cambridge Earth science series, Cambridge University Press.
108. Loren Kroenke, R.S., et al., West side of the Parece Vela Basin, in Initial Reports of the Deep Sea Drilling Projects, Volume LIX. 1981. p. 320-335.
109. 周墨清, 太平洋中部磁性地层学研究. 海洋地质与第四纪地质, 1995. 15(1): p. 41-56.
110. Mull R, M.D., Geomagnetic reversals. Geotimes, 1989. 20( 20).
111. 丛友滋、李素玲、程国良等, 黄海两钻孔岩芯的古地磁分析. 地震地质, 1980. 2(3): p. 64-69.
112. 小山真人,沈耀龙译, 据古地磁资料探讨菲律宾海板块构造发育史. 地学杂志, 1991. 4.
113. 李粹中, 南海深海短柱样的磁性地层学特征. 沉积学报, 1994. 12(3): p. 136-142.
114. Horng C S, R.A.P., Liang W T., A 2.14Myr astronomically tuned record of relative geomagnetic paleointensity from the western Pillippine Sea. Journal of Geophysical Research, 2003. 108(B1): p. 1-15.
115. 季军良、郑洪波、刘锐等, 邙山黄土地层再研究. 海洋地质与第四纪地质, 2004. 24(4): p. 101-109.
116. Reynolds R L, K.J.W., Magnetic records of climate change. Rev.Geophys,Supplement, 1995: p. 101-110.
117. 鹿化煜、安芷生, 洛川黄土粒度组成的古气候意义. 科学通报, 1997. 42(1): p. 66-69.
118. 李军、高抒、孙有斌等, 冲绳海槽南部沉积层序的粒度特征. 沉积学报, 2003. 21(3): p. 461-467.
119. 杨小强、李华梅, 泥河湾盆地沉积物粒度组分与磁化率变化相关性研究. 沉积学报, 2002. 20(4): p. 675-680.
120. 杨小强、李华梅, 泥河湾盆地沉积物磁化率及粒度参数对沉积环境的响应. 沉积学报, 1999. 17(增刊): p. 763-769.
121. Taylor RM, M.B., Self PG, Magnetite in soils: the synthesis of single-Domain and superparamagnetic magnetite. Clay Minerals, 1987. 22: p. 411-422.
122. 韩晓非、张卫国、陈满荣等, 长江口潮滩植物对沉积物铁的地球化学循环及磁性特征的影响. 沉积学报, 2003. 21(3): p. 495-500.
123. 张卫国、俞立中、陆敏, 长江口潮滩沉积物氧化铁与磁性特征的关系. 地
球物理学报, 2003. 46(1): p. 79-86.