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Journal articles on the topic 'Palaeomagnetic study'

Author: Grafiati

Published: 6 September 2023

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1

Tiano, Pasquale, Alberto Incoronato, and Donald H. Tarling. "Palaeomagnetic study on Vesuvius lava flows." Geophysical Journal International 163, no. 2 (2005): 518–26. http://dx.doi.org/10.1111/j.1365-246x.2005.02768.x.

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2

Thouveny, N. "High-resolution palaeomagnetic study of Late Pleistocene sediments from Baffin Bay:first results." Canadian Journal of Earth Sciences 25, no. 6 (1988): 833–43. http://dx.doi.org/10.1139/e88-082.

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The detailed palaeomagnetic study of core 85027016, collected in central Baffin Bay, confirms the occurrence of anomalous directions in the depositional remanent magnetization, previously observed in the upper part of the Pleistocene sequence. Chronology and sedimentation rates are discussed on the basis of new 14C ages, 18O isotopic stratigraphy, and palaeoclimatic arguments provided by other works. Two successions of anomalous inclinations are recorded between 15 000 and 30 000 years BP, preceded by long-period secular variations. The possible occurrence of geomagnetic excursions in this reg

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3

Taylor, G. K. "A palaeomagnetic study of a Caledonian ophiolite." Geophysical Journal International 94, no. 1 (1988): 157–66. http://dx.doi.org/10.1111/j.1365-246x.1988.tb03435.x.

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4

Yan, Yonggang, Qian Zhao, Donghai Zhang, Punya Charusiri, Baochun Huang, and Peizhen Zhang. "Palaeomagnetism of Late Triassic volcanic rocks from the western margin of Khorat Basin, Thailand and its implication for ambiguous inclination shallowing in Mesozoic sediments of Indochina." Geophysical Journal International 219, no. 2 (2019): 897–910. http://dx.doi.org/10.1093/gji/ggz331.

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SUMMARY Palaeomagnetic constraints are essential factors in the reconstruction of the Mesozoic convergence of Eastern Asia blocks. As one of the key blocks, Indochina was constrained only by sedimentary-rocks-derived palaeomagnetic data. To evaluate whether the palaeomagnetic data used to restore the Late Triassic position of Indochina suffered inclination shallowing effects, we conducted a palaeomagnetic and geochronologic study on a coeval volcanic clastic rocks sequence in the western margin of the Khorat Basin, Thailand. The U-Pb SIMS dating on zircons indicates the age of the sampling sec

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5

Darabi, M. H., and J. D. A. Piper. "Palaeomagnetic study of the Canisp Porphyry, NW Scotland: an Early Silurian palaeomagnetic pole from the Laurentian Foreland." Scottish Journal of Geology 40, no. 1 (2004): 83–92. http://dx.doi.org/10.1144/sjg40010083.

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6

Jele ska, M., and M. Lewandowski. "A palaeomagnetic study of Devonian sandstone from Central Spitsbergen." Geophysical Journal International 87, no. 2 (1986): 617–32. http://dx.doi.org/10.1111/j.1365-246x.1986.tb06641.x.

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7

Garde, S. C., and I. O. Ayeni. "A palaeomagnetic study of Cainozoic basalts from Northern Nigeria." Geophysical Journal International 106, no. 3 (1991): 717–23. http://dx.doi.org/10.1111/j.1365-246x.1991.tb06344.x.

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8

Bylund, Göuran, and Erik Halvorsen. "Palaeomagnetic Study of Mesozoic Basalts From Scania, Southernmost Sweden." Geophysical Journal International 114, no. 1 (1993): 138–44. http://dx.doi.org/10.1111/j.1365-246x.1993.tb01473.x.

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9

Hlavatskyi, D. V. "Refined magnetostratigraphic position of the Shyrokyne unit in loess sequences from Central Ukraine." Journal of Geology, Geography and Geoecology 28, no. 2 (2019): 301–12. http://dx.doi.org/10.15421/111930.

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The youngest geomagnetic polarity reversal, the Matuyama–Brunhes boundary (MBB), which occurred 780 kyr ago, is a “golden spike” in the age calibration of sediment sequences. The use of palaeomagnetic method as a stratigraphic tool in the study of loess sequences from Ukraine originated some 50 years ago. One major problem in using the available data is the contradictory position of the MBB in different stratigraphic units, which affected historic evolution of thechronostratigraphic models of the Quaternary in Ukraine. The most important units in this regard are the Shyrokyne and Martonosha un

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10

Hlavatskyi, D. V., Y. M. Veklych, V. G. Bakhmutov, et al. "Palaeomagnetic suitability of a new section with a potential lower boundary for the Quaternary on the left bank of the lower River Danube." Geofizicheskiy Zhurnal 44, no. 4 (2022): 38–50. http://dx.doi.org/10.24028/gj.v44i4.264840.

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A first palaeomagnetic study has been carried out on a new section with a potential lower boundary interval for the Quaternary, Dolynske 3. Recently, the Matuyama-Brunhes boundary (at 780 ka) was detected in the adjacent section of Dolynske 2. The current study focuses on the hydromorphic palaeosols, loesses and pedosediments of the Bogdanivka to Kryzhanivka units. Taking into account previous palaeomagnetic data from other sections of the loess/soil formation of Ukraine, the Gauss-Matuyama boundary (2.58 Ma) could be expected to be at the top of the Bogdanivka soil unit. However, rock magneti

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11

Elming, Sten-ÅKe. "A palaeomagnetic study of Svecokarelian basic rocks from northern Sweden." Geologiska Föreningen i Stockholm Förhandlingar 107, no. 1 (1985): 17–35. http://dx.doi.org/10.1080/11035898509452608.

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12

Iosifidi, A. G., S. Bogdanova, A. N. Khramov, and G. Bylund. "Palaeomagnetic study of Palaeoproterozoic granitoids from the Voronezh Massif, Russia." Geophysical Journal International 137, no. 3 (1999): 723–31. http://dx.doi.org/10.1046/j.1365-246x.1999.00818.x.

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13

Villasante-Marcos, V., M. L. Osete, F. Gervilla, and V. García-Dueñas. "Palaeomagnetic study of the Ronda peridotites (Betic Cordillera, southern Spain)." Tectonophysics 377, no. 1-2 (2003): 119–41. http://dx.doi.org/10.1016/j.tecto.2003.08.023.

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14

Belluso, Elena, and Roberto Lanza. "Palaeomagnetic results from the middle Tertiary Meander Intrusives of northern Victoria Land, East Antarctica." Antarctic Science 8, no. 1 (1996): 61–72. http://dx.doi.org/10.1017/s0954102096000107.

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The Tertiary stocks (Meander Intrusives) cropping out along the coasts of the Ross Sea were sampled for a palaeomagnetic study during the sixth Italian expedition to northern Victoria Land. Laboratory investigations concerned magnetic mineralogy and remanent magnetization. Minerals of the magnetiteulvöspinel series occur in the rocks from all stocks, with low-Ti titanomagnetite usually prevalent. Haematite and goethite occur in small amounts as alteration products. Large secondary components commonly screen the characteristic remanent magnetization and were removed by thermal or AF demagnetiza

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15

Rodríguez-Trejo, A., L. M. Alva-Valdivia, M. Perrin, G. Hervé, and N. López-Valdés. "Analysis of geomagnetic secular variation for the last 1.5 Ma recorded by volcanic rocks of the Trans Mexican Volcanic Belt: new data from Sierra de Chichinautzin, Mexico." Geophysical Journal International 219, no. 1 (2019): 594–606. http://dx.doi.org/10.1093/gji/ggz310.

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Summary The great wealth of volcanism along the Trans Mexican Volcanic Belt (TMVB) and the need to improve the secular variation curve of the Earth magnetic field of the region is the aim of this research. 300 oriented cores from 33 sites and 21 individual cooling units were acquired from Sierra de Chichinautzin volcanic field (ChVF) and Sierra de Santa Catarina (SSC). Directional analysis and rock magnetic experiments were performed (e.g. thermal demagnetization, hysteresis loop, susceptibility vs temperature), achieving 21 new averaged palaeomagnetic directions. New results are consistent wi

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16

Αηδονά, Ε., Δ. Κοντοπούλου, and R. Scholger. "RE-ORIENTANTION METHODS OF CORE SAMPLES: IMPLICATIONS TO SEDIMENT CORES FROM N. GREECE." Bulletin of the Geological Society of Greece 36, no. 3 (2004): 1194. http://dx.doi.org/10.12681/bgsg.16462.

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The different methods of re-orientation of core samples are discussed in the present study. In order to obtain results from core samples concerning the direction of the formation, their permeability and their anisotropy, it is essential first to bring all the pieces of the core into their initial position with regard to the North and to the horizontal (in-situ). In this study we emphasize particularly to the palaeomagnetic technique. This re-orientation method uses the magnetic components of the rocks (especially the viscous component) in order to determine the direction with regard to the Nor

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17

Roger, J., S. Sen, H. Thomas, C. Cavelier, and Z. Al Sulaimani. "Stratigraphic, palaeomagnetic and palaeoenvironmental study of the Early Oligocene vertebrate locality of Taqah (Dhofar, Sultanate of Oman)." Newsletters on Stratigraphy 28, no. 2-3 (1993): 93–119. http://dx.doi.org/10.1127/nos/28/1993/93.

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18

Hong, Zhu, Yang Guanxiu, and Sheng Axing. "Palaeomagnetic Study of Permian Strata at the Yuzhou-Dafengkou Section, Henan." Acta Geologica Sinica - English Edition 9, no. 4 (2009): 356–65. http://dx.doi.org/10.1111/j.1755-6724.1996.mp9004003.x.

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19

Otofuji, Y., Y. Inoue, S. Funahara, F. Murata, and X. Zheng. "Palaeomagnetic study of eastern Tibet-deformation of the Three Rivers region." Geophysical Journal International 103, no. 1 (1990): 85–94. http://dx.doi.org/10.1111/j.1365-246x.1990.tb01754.x.

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20

Piper, J. D. A. "Palaeomagnetic study of the Nagssugtoqidian mobile belt in Central-West Greenland." Precambrian Research 28, no. 1 (1985): 75–110. http://dx.doi.org/10.1016/0301-9268(85)90075-0.

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21

Elming, Sten-Åke, Mohsen Oveisy Moakhar, and Ol Of Martinsson. "A palaeomagnetic and geochemical study of basic intrusions in northern Sweden." GFF 126, no. 2 (2004): 243–52. http://dx.doi.org/10.1080/11035890401262243.

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22

Vizán, Haroldo, Peter Turner, John A. Millson, and Rob A. Ixer. "Palaeomagnetism of the Mahatta Humaid Group (Cambrian – Early Ordovician, Oman), including a re-interpretation of previous Neoproterozoic palaeomagnetic data." GeoArabia 14, no. 2 (2009): 71–96. http://dx.doi.org/10.2113/geoarabia140271.

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ABSTRACT We carried out a palaeomagnetic study in the Al-Huqf region (Sultanate of Oman) on rocks that belong to different units of the Cambrian – Ordovician Mahatta Humaid Group. Thirty-nine samples were systematically collected from a succession ca. 520–495 Ma old. Seventeen samples showed characteristic remanent magnetization components with two antipodal polarities carried by hematite. Evidence suggests that these components have a primary origin. A detailed petrographic analysis revealed syntaxial overgrowths parallel to the easy plane of magnetization of the magnetic carriers that has pr

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23

IZQUIERDO-LLAVALL, ESTHER, ANTONIO CASAS-SAINZ, BELÉN OLIVA-URCIA, and ROBERT SCHOLGER. "Palaeomagnetism and magnetic fabrics of the Late Palaeozoic volcanism in the Castejón-Laspaúles basin (Central Pyrenees). Implications for palaeoflow directions and basin configuration." Geological Magazine 151, no. 5 (2013): 777–97. http://dx.doi.org/10.1017/s0016756813000769.

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AbstractThe Castejón-Laspaúles basin is one of the South Pyrenean basins of Late Variscan age that were strongly inverted during the Alpine compression (Late Cretaceous–Tertiary). It is mainly composed by Stephanian pyroclastic and volcanic deposits that reach a maximum thickness of ~ 500 m, and are overlain by Permian and Triassic sedimentary units. A palaeomagnetic and magnetic fabrics (AMS) study was carried out in the Stephanian units, where the general absence of flow markers at the outcrop scale and the Alpine inversional structure prevent the straightforward reconstruction of the origin

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24

Kondopoulou, D., I. Zananiri, A. Michard, et al. "NEOGENE TECTONIC ROTATIONS IN THE VICINITY OF THE NORTH AEGEAN TROUGH: NEW PALAEOMAGNETIC EVIDENCE FROM ATHOS AND SAMOTHRAKI (GREECE)." Bulletin of the Geological Society of Greece 40, no. 1 (2018): 343. http://dx.doi.org/10.12681/bgsg.16590.

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The present study focuses on two post-orogenic plutons, the Athos (Grigoriou) and Samothraki granites, as well as the Samothraki volcanics, located in the vicinity of the North Aegean Trough. A detailed palaeomagnetic study was carried out, with the aim of constraining the age and mechanism of tectonic rotations. In addition, anisotropy of low field magnetic susceptibility (AMS) was studied and isothermal remanent magnetization (IRM) and thermomagnetic analyses were performed. Finally, a radiometric age for the Athos granite was obtained (43.3 ± 1.0 Ma K/Ar biotite). The measured declinations

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25

Satolli, Sara, Simone Agostini, and Fernando Calamita. "Behaviour of minor arcuate shapes hosted in curved fold-and-thrust belts: an example from the Northern Apennines (Italy)." Geological Magazine 156, no. 9 (2019): 1547–64. http://dx.doi.org/10.1017/s0016756818000845.

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AbstractArcuate fold-and-thrust belts have been extensively studied in the literature. Less attention, however, has been paid to the characteristics of local-scale arcuate structures, meaning 5–10 km long fold or thrust traces that display map-view curvature. Nevertheless, detailed investigation of small arcuate structures hosted in major arcs can contribute to understanding the pervasiveness of deformation mechanisms. We performed a combined geological and palaeomagnetic study on 21 sites from ac. 60 km2area in the Northern Apennines in order to analyse minor arcs at a kilometric scale. As ev

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26

Abou Deeb, J. M., M. M. Otaki, D. H. Tarling, and A. L. Abdeldayem. "A palaeomagnetic study of Syrian volcanic rocks of Miocene to Holocene age." Geofísica Internacional 38, no. 1 (1999): 17–26. http://dx.doi.org/10.22201/igeof.00167169p.1999.38.1.896.

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Rocas volcánicas del Mioceno y más jóvenes de varias localidades de Siria muestran polaridades normales y reversas después de desmagnetización térmica. Las similitudes en las direcciones medias de magnetización pueden ser usadas para establecer correlación entre lavas. Las polaridades observadas sugieren que algunas de las lavas del Cuaternario son más antiguas de lo propuesto en cartografías previas. Los sitios con direcciones medias reversas e intermedias presentan una dispersión angular mayor que la observada en los sitios de direcciones normales. La dispersión media global es mayor que la

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27

Juárez, M. T., M. L. Osete, R. Vegas, C. G. Langereis, and G. Meléndez. "Palaeomagnetic study of Jurassic limestones from the Iberian Range (Spain): tectonic implications." Geological Society, London, Special Publications 105, no. 1 (1996): 83–90. http://dx.doi.org/10.1144/gsl.sp.1996.105.01.07.

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28

Shcherbakova, V. V., V. G. Bakhmutov, V. P. Shcherbakov, G. V. Zhidkov, and V. V. Shpyra. "Palaeointensity and palaeomagnetic study of Cretaceous and Palaeocene rocks from Western Antarctica." Geophysical Journal International 189, no. 1 (2012): 204–28. http://dx.doi.org/10.1111/j.1365-246x.2012.05357.x.

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29

Channell, J. E. T., C. McCabe, and N. H. Woodcock. "Palaeomagnetic study of Llandovery (Lower Silurian) red beds in north-west England." Geophysical Journal International 115, no. 3 (1993): 1085–94. http://dx.doi.org/10.1111/j.1365-246x.1993.tb01511.x.

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30

Harcombe-Smee, B. J., J. D. A. Piper, T. C. Rolph, and D. N. Thomas. "A palaeomagnetic and palaeointensity study of the Mauchline lavas, south-west Scotland." Physics of the Earth and Planetary Interiors 94, no. 1-2 (1996): 63–73. http://dx.doi.org/10.1016/0031-9201(95)03083-2.

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31

Jackson, K. C. "A palaeomagnetic study of Apennine thrusts, Italy: Monte Maiella and Monte Raparo." Tectonophysics 178, no. 2-4 (1990): 231–40. http://dx.doi.org/10.1016/0040-1951(90)90149-3.

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32

Poornachandra Rao, G. V. S., and J. Mallikharjuna Rao. "A palaeomagnetic study of charnockites from Madras Block, Southern Granulite Terrain, India." Gondwana Research 10, no. 1-2 (2006): 57–65. http://dx.doi.org/10.1016/j.gr.2005.11.015.

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33

Xu, T. C., and D. H. Tarling. "A palaeomagnetic study of the intrusions and Carboniferous sediments at Dunbar, Scotland." Scottish Journal of Geology 23, no. 1 (1987): 39–48. http://dx.doi.org/10.1144/sjg23010039.

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34

Márton, E., and L. Fodor. "Combination of palaeomagnetic and stress data—a case study from North Hungary." Tectonophysics 242, no. 1-2 (1995): 99–114. http://dx.doi.org/10.1016/0040-1951(94)00153-z.

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35

Dannemann, Sven, Erwin Appel, Wolfgang Rösler, Udo Neumann, Ursina Liebke, and Debarati Nag. "Palaeomagnetic indication for India–Asia collision at 12°N and maximum 810 km Greater India extent in the western suture zone." Geophysical Journal International 229, no. 2 (2022): 1193–211. http://dx.doi.org/10.1093/gji/ggab528.

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SUMMARY Knowing the pre-collisional extent of the northern Indian Plate margin (‘Greater India’) is vital to understanding the tectonic evolution of the India–Asia collision and the formation of the Himalayan–Tibetan orogen. However, suitable geological units for palaeomagnetic investigations along the Himalayan belt are limited, which makes it difficult to reconstruct Greater India during the pre-collisional period in Late Cretaceous to Palaeogene. Often the palaeomagnetic results from the Zongpu Formation at Gamba in southern Tibet (∼88.5°E) were used for estimates of Greater India, but thei

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36

DARABI, M. H., and J. D. A. PIPER. "Palaeomagnetism of the (Late Mesoproterozoic) Stoer Group, northwest Scotland: implications for diagenesis, age and relationship to the Grenville Orogeny." Geological Magazine 141, no. 1 (2004): 15–39. http://dx.doi.org/10.1017/s0016756803008148.

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The Stoer is the lowest of three groups comprising the Torridonian Supergroup, a clastic succession deposited late in Mesoproterozoic times on the (Lewisian) metamorphic foreland to the Caledonian Orogen in northwest Scotland. This study reports a palaeomagnetic, rock magnetic and magnetic fabric investigation through the full stratigraphic thickness of the succession. A primary magnetic fabric of sedimentary origin defines current flow from a westerly veering to northwesterly source. Rock magnetic studies identify the presence of both magnetite and hematite in these sediments. Magnetite is ap

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37

KAYMAKCI, N., E. ALDANMAZ, C. LANGEREIS, T. L. SPELL, O. F. GURER, and K. A. ZANETTI. "Late Miocene transcurrent tectonics in NW Turkey: evidence from palaeomagnetism and 40Ar–39Ar dating of alkaline volcanic rocks." Geological Magazine 144, no. 2 (2007): 379–92. http://dx.doi.org/10.1017/s0016756806003074.

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A number of intra-continental alkaline volcanic sequences in NW Turkey were emplaced along localized extensional gaps within dextral strike-slip fault zones prior to the initiation of the North Anatolian Fault Zone. This study presents new palaeomagnetic and 40Ar–39Ar geochronological results from the lava flows of NW Turkey as a contribution towards understanding the Neogene–Quaternary tectonic evolution of the region and possible roles of block rotations in the kinematic history of the region. 40Ar–39Ar analyses of basalt groundmass indicate that the major volume of alkaline lavas of NW Turk

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38

Thistlewood, L., and M. A. Whyte. "A palaeomagnetic and mineral magnetic study of the Speeton Shell Bed, North Yorkshire." Proceedings of the Yorkshire Geological Society 49, no. 4 (1993): 325–34. http://dx.doi.org/10.1144/pygs.49.4.325.

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39

Qizhong, Liang, Fang Wu, and Rob Van der Voo. "Palaeomagnetic Study on the Precambrian-Cambrian Boundary Candidate Stratotype Section at Meishucun, Yunnan." Acta Geologica Sinica - English Edition 4, no. 1 (2009): 97–109. http://dx.doi.org/10.1111/j.1755-6724.1991.mp4001009.x.

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40

Taylor, G. K. "A palaeomagnetic study of two Precambrian-Cambrian dyke swarms from the Armorican Massif." Geological Society, London, Special Publications 51, no. 1 (1990): 69–80. http://dx.doi.org/10.1144/gsl.sp.1990.051.01.05.

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41

Fossen, Mickey C. Van, and Dennis V. Kent. "A Palaeomagnetic Study of 143 Ma Kimberlite Dikes In Central New York State." Geophysical Journal International 113, no. 1 (1993): 175–85. http://dx.doi.org/10.1111/j.1365-246x.1993.tb02538.x.

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42

Eggler, D. H., and E. E. Larson. "Palaeomagnetic Study of Dated Pre-Cambrian Rocks of the Front Range, Colorado-Wyoming." Geophysical Journal of the Royal Astronomical Society 14, no. 1-4 (2010): 497–504. http://dx.doi.org/10.1111/j.1365-246x.1967.tb06269.x.

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43

Elming, S. A., P. Layer, and K. Ubieta. "A palaeomagnetic study and age determinations of Tertiary rocks in Nicaragua, Central America." Geophysical Journal International 147, no. 2 (2001): 294–309. http://dx.doi.org/10.1046/j.0956-540x.2001.01526.x.

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44

Mushayandebvu, M. F., D. L. Jones, and J. C. Briden. "A palaeomagnetic study of the Umvimeela Dyke, Zimbabwe: evidence for a Mesoproterozoic overprint." Precambrian Research 69, no. 1-4 (1994): 269–80. http://dx.doi.org/10.1016/0301-9268(94)90091-4.

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45

Sherwood, Graham J., and S. Basu Mallik. "A palaeomagnetic and rock magnetic study of the northern Rajmahal Volcanics, Bihar, India." Journal of Southeast Asian Earth Sciences 13, no. 2 (1996): 123–31. http://dx.doi.org/10.1016/0743-9547(96)00013-x.

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46

Hlavatskyi, D. V., V. N. Stepanchuk, D. M. Kuzina, et al. "Rock magnetic and palaeomagnetic studies of loess-palaesol sections — Lower Palaeolithic sites within the Southern Bug Valley (Medzhybizh, Holovchyntsi)." Geofizicheskiy Zhurnal 43, no. 1 (2021): 3–37. http://dx.doi.org/10.24028/gzh.0203-3100.v43i1.2021.225539.

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Combined rock magnetic and palaeomagnetic studies of loess-soil sections — Lower Paleolithic sites in the valley of the Southern Bug (Medzhybizh, Holovchintsi) — have been performed for the first time in order to determine the suitability of these objects for palaeomagnetic study and the establishment of magnetostratigraphic markers. Investigated sections by rock magnetic characteristics are closest to the sections of the Volynian Upland, and refer to the intermediate «Chinese» type of formation of magnetic properties, with an admixture of the «Alaskan» mechanism. These sections are characteri

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47

Gibert, J., Ll Gibert, A. Iglesias, and E. Maestro. "Two ‘Oldowan’ assemblages in the Plio-Pleistocene deposits of the Orce region, southeast Spain." Antiquity 72, no. 275 (1998): 17–25. http://dx.doi.org/10.1017/s0003598x00086233.

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Stone artefacts reported from the Orce region (Grenada, Spain) indicate a first human presence in western Europe as early as the Plio-Pleistocene boundary, making a ‘long chronology’ for European hominids against the claims for a briefer human presence. Excavations of Barranco León-5 and Fuentenueva-3a in 1995 have produced two groups of lithic artefacts of ‘Oldowan’ type, seen as the most ancient of western Europe by faunal associations and palaeomagnetic study.

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48

Idnurm, M., and C. A. Heinrich. "A palaeomagnetic study of hydrothermal activity and uranium mineralization at Mt Painter, South Australia." Australian Journal of Earth Sciences 40, no. 1 (1993): 87–101. http://dx.doi.org/10.1080/08120099308728065.

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49

Incoronato, A., D. H. Tarling, and G. Nardi. "Palaeomagnetic study of an allochthonous terraine: the Scisti Silicei Formation, Lagonegro Basin, southern Italy." Geophysical Journal International 83, no. 3 (1985): 721–29. http://dx.doi.org/10.1111/j.1365-246x.1985.tb04334.x.

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Rey, D., P. Turner, and A. Yaliz. "Palaeomagnetic study and magnetostratigraphy of the Triassic Skagerrak Formation, Crawford Field, UK North Sea." Geological Society, London, Special Publications 73, no. 1 (1993): 399–420. http://dx.doi.org/10.1144/gsl.sp.1993.073.01.23.

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