|
|
|
| 塔里木板块柯坪地区晚石炭世、早二叠世岩石的磁性组构研究及其意义 |
| 金国海1, 吴能友1, 方大钧1, 许同春2, 葛同明3 |
1. 浙江大学地球科学系, 杭州 310027;
2. 国家地震局地球物理研究所, 北京 100083;
3. 地矿部广州海洋地质调查局, 广州 510760 |
|
| A STUDY ON ANISOTROPY OF MAGNETIC SUSCEPTIBILITY OF LATE CARBONIFEROUS AND EARLY PERMIAN ROCKS FROM KEPING AREA OF TARIM PLATE AND ITS INTERPRETATION IN THE LIGHT OF STRAIN |
| Jin Guohai1, Wu Nengyou1, Fang Dajun1, Xu Tongchun2, Ge Tongming3 |
1. Department of Earth Sciences, Zhejing University, Hangzhou 310027;
2. Institute of Geophysics, State Seismological Bureau, Beijing 100083;
3. Guangzhou Marine Geological Survey, Guangzhou 510760 |
| 引用本文: |
金国海, 吴能友, 方大钧, 许同春, 葛同明. 塔里木板块柯坪地区晚石炭世、早二叠世岩石的磁性组构研究及其意义[J]. 物探与化探, 1995, 19(1): 68-73.
Jin Guohai, Wu Nengyou, Fang Dajun, Xu Tongchun, Ge Tongming. A STUDY ON ANISOTROPY OF MAGNETIC SUSCEPTIBILITY OF LATE CARBONIFEROUS AND EARLY PERMIAN ROCKS FROM KEPING AREA OF TARIM PLATE AND ITS INTERPRETATION IN THE LIGHT OF STRAIN. Geophysical and Geochemical Exploration, 1995, 19(1): 68-73.
|
|
|
|
| 链接本文: |
|
https://www.wutanyuhuatan.com/CN/
或
https://www.wutanyuhuatan.com/CN/Y1995/V19/I1/68
|
| ［1］ 许同春,磁组构,地震地磁观测与研究,1989.
［2］ Rathore, J. S., The magnetic fabric of Bone slates frem the sorrowdale vclvanic group in the English Lake District and their corrlations with serain, Tectonophysics, 67. 207-220, 1980.
［3］ Rathore, J, S., Magnetic suscepribility anisotrogy in the Cambrian slate belt of North Wales and correlation with strain, Tectonophysics, 53, 88-97, 1979.
［4］ Hscuda, F.Magoesic anisotropy of rocks and its application in geology and geophysics. Geophys.Surv.,5,37, 82, 1882.
［5］ Cogne, J. P., Perroud, H., Texicr,从.P. and Bonhommet, N., Strain reorientation of hematite and its bearing upon remancnt magnetization, Tectonics, 5, 753-767, 1986.
［6］ Li, Z. X., Schmidt, P. W., Embleton, B. J. J., Paleomagnetism of the Hervey Group, Central N. S. W.,and its tectonic implications, Tectonics, 7, 351-367, 1988.
［7］ Noel, M., The magetic remanencee and anisotropy of susceptibility of cave sediments from Agen Allwedd South Wales, Geophys. J. R. astr. Soc., 72, 557-570, 1983.
［8］ Schieber, J. and Ellwood, B. B., The coincidence of macroscopic paleocurrent indicators and magnetic lineation in shales from the Precambrian belt basin, Journal of Sedimentary Petrology, 58, 830-835,1988.
［9］ Ellwood, B, B., Estimates of flow direction for Calcalkaline Weldded Stuff and magnetic susceptihi-lity measurements: central San Juan Mountains, Southwest Colorado, Earth Plant. Sci. Lett., 59,303-314,1982.
［10］ Kligfield, R., Vwens, W. H, and Lowrie, W., Magnetic suscepbility anisotropy, strain, and progressive deformation in Permian sediments from the Maritime Alpes ［11］ Hirt, A. M., Lowrie, W. and Pfiffner, O. A., A paleomagnetic study of tectonically deformed red beds df the Lower Glarus Nappe Complez. Eastern Switzerland, Tectonics, 5, 723-731, 1986,
［12］ MacDonald, W. D. and Ellwood, B. B., Anisotropy of magnetic susceptibility: sedimentological, igneous and structuraltectonic applications, Geophys. Rev., 5, 905-909, 1987.
［13］ Ramsay, J. G., Folding and fracturing of rocks, McGraw-Hill, Newyork, 568pp, 1967.
［14］ Kligfield, R., lowrie, W., Hirt, A. and Siddans, A. W. B., Effect of progressive deformation on rema-ncnt magnetization of Permian redheds from the Alpes Maritimes (France),Tectonophysics, 40, 287-308, 1983. |
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
| |
Shared |
|
|
|
|
| |
Discussed |
|
|
|
|
