Various magnetic minerals and each other, s transformation phenomena exist in carbonate rocks .Magnetic minerals produced in the each stage of the sedimentation evolusion process of the rocks carry information about the palaeoenvironment in their occurrence,thus they become direct objects of study in sedimentary palaeogeography and environment magnetism.Magnetic minerals derive primary remanent magnetization from the geomagnetic field during their diagenesis.It is prereguisite for gaining the reliable palaeomagnetic data,which are used for working out polar wander paths,drawing up palaeogeography maps with nonpresent boundaries and working the palaeogeographic reconstruction,correctly to identify them and to distinguish remanent magnetism components of all kinds.Thus,they become the major objects of study in palaeomagnetism and tectonic palaeogeography.In the epigenesis stage,magnetic minerals into which is usually translated by the primitive ones are often caused by tectonic movement or by the magmatism and the fluid medium activity relating to it .New magnetic minerals carry some information about remagnetized remanent magnetization .Thus,they should similarly be the major objects of study in palaeomagnetism and tectonic palaeogeography. We will offer more reliable and abundant palaeomagnetism data to people for working the palaeogeographic reconstruction if we collect more samples relative to the tectonic event and the thermal event and advance the minerageny study for magnetic minerals.It follows that the tight relation between magnetic minerals and the study on palaeogeography reguires our close attention though palaeogeography,a highly comprehensive branch of geoscience, has evolved into several branches.
About author: Xu Heling,born in 1944,graduated from Beijing College of Geology in 1965.Now he is a professor of the Institute of Geomechanics CAGS and engages in environmental mineralogy and stress mineralogy.
Cite this article:
. MAGNETIC MINERALS IN CARBONATE ROCKS AND ITS ROLE IN PALEOGEOGRAPHIC STUDY[J]. JOURNAL OF PALAEOGEOGRAPHY, 2000, 2(3): 75-82.
. MAGNETIC MINERALS IN CARBONATE ROCKS AND ITS ROLE IN PALEOGEOGRAPHIC STUDY[J]. JOPC, 2000, 2(3): 75-82.
1 Berner R A. Occurrence of sedimentary pyrite.American Journal of Science, 1970, 268(1): 13- 23
2 中国科学院矿床地球化学开放研究实验室. 矿床地球化学. 北京:地质出版社,1997,275-278
3 冯增昭,王英华,刘焕杰等. 中国沉积学. 北京:石油工业出版社,1994. 31
4 Curris C D, Spears D A. Occurrence of sedimentery iron minerals. Economic. Geology, 1968, 63(3): 257-262
5 刘英俊,曹励明,李兆麟等. 元素地球化学. 北京:科学出版社,1984. 95-96
6 Tarling D H. Paleomagnetism. London: Chapman and Hall, 1983. 50
7 王 濮,潘兆橹,翁玲宝等. 系统矿物学(上册). 北京:地质出版社,1982. 345
8 冯增昭. 我国古地理学的形成、发展与展望. 古地理学报,1(2):1-7
9 王鸿祯,刘本培.《中国古地理图集》的历史背景和前途展望. 古地理学报,1(2):92-96
10 Verosub K L, Roberts A P. Environmental magnetism: Past, present and future. J. Geophys. Res., 1995, 100: 2175-2192
11 朱日祥等。中国主要地块显生宙古地磁视极移曲线与地块运动. 中国科学(D辑),1998,
28(增刊):1-16
12 马醒华,杨振宇. 中国三大地块的碰撞拼合与欧亚大陆的重建. 地球物理学报,1993, 34(6):476-481
13 Van der Voo R. Phanerozoic paleomagnetic poles from Europe and North America and comparison with continental reconstructions. Reviews Geophys, 1990, 28: 167-206
14 Fuller M, Cisowski S, Hart M et al. NRM(s)demagnetization plot: An aid to the interpretation of natural remanent magnetization. Geophys Res Lett, 1988, 15: 518-521
15白立新,朱日祥. 扬子地块古生代大地构造演化及古地磁研究综述. 地球物理学进展,1996,11(3):55-67
16 McCabe C, Sassen R, Saffer B. Occurrence of secondary magnetite within biodegraded oil.Geology, 1987, 15 (1): 7-10
17 Elmore R D, Engel M H, Crawford L et al. Evidence for a relationship between hydrocarbons and authigenic magnetite. Nature, 1987, 325: 428-430
18谈晓冬,方大钧,王明岩等. 塔里木盆地北部中、新生代钻孔岩芯古地磁研究-喜山期岩石重磁化与油气移聚.地球物理学报,1995,38(5):688-691
19刘庆生,刘树根. 塔北雅克拉油田储层岩石的磁性与矿物学特征及其意义. 科学通报,1997,42(24):2639-2642
20 Shen Z Y, Fang D. Magnetite of early Ordovician limestone in Tarim and implications for Paleomagnetism. Chinese Science Bulletin, 1997, 42 (13): 1110-1113
21 Suk D, Peacor D R, Van der Voo R. Replacement of pyrite framboids by magnetite in limestone and implications for paleomagnetism. Nature, 1990. 345: 611-613
22杨振宇. 泰国Khorat盆地二叠纪石灰岩的重磁化研究.地球物理学报,1996,39(增刊):173-181
23徐和聆,马醒华,陈克樵. 重磁化碳酸盐岩中磁性矿物相变特征分析. 中国科学(D辑),1999,29(4):347-350
24 McCabe C,Sassen R,Saffer B. Occurrence of secondary magnetite whthin biodegraded oil.Geology,1987,15(1):7-10