[1]
Dai, Y.P., Zhang, L.C., Wang, C.L., Liu, L., Cui, M.L., Zhu, M.T. and Xiang, P. (2012) Genetic Type, Formation Age and Tectonic Setting of Waitoushan Banded Iron Formation, Benxi, Liaoning Province. Acta Petrologica Sinica, 28, 3574-3594.
[2]
Feng, J.R., Zhou, Z.H. and Xiao, R.G. (2009) The Protolith Restoration of the Second Diggings Wall Rock in Gongchangling Iron Ore, Liaoning Province. China Mining Magazine, 18, 106-110.
[3]
Liu, J. and Jin, S.Y. (2010) Geochemical Characteristics and Original Rock Restoration of Plagioclase Amphibolites in the Gongchangling Iron Deposit, Liaoning Province. Geology in China, 37, 324-333.
[4]
Cui, P.L., Sun, J.G., Zhang, P., Gu, A.L., Zhou, K.Q. and Sun, Q.L. (2012) Geochemical Study on BIF Wall Rock— Plagioclase Amphibolites of Cigou Formation in Anshan-Benxi Area. Mineral Deposits, 31, 93-94.
[5]
Zhang, P., Yang, H.Z., Zhou, Y. and Shi, J.M. (2013) Geochemical Characters and Geological Significance of Plagioclase Amphibolites from Anshan Group Cigou Formation, Anshan-Benxi Area. Geological Review, 59, 1217-1218.
[6]
Sun, X.H., Zhu, X.Q., Tang, H.S., Zhang, Q., Luo, T.Y. and Han, T. (2014) Protolith Reconstruction and Geochemical Study on the Wall Rocks of Anshan BIFs, Northeast China: Implications for the Provenance and Tectonic Setting. Journal of Geochemical Exploration, 136, 65-75.
http://dx.doi.org/10.1016/j.gexplo.2013.10.009
[7]
Wang, E.D., Xia, J.M., Zhao, C.F., Fu, J.F. and Hou, G.Q. (2013) Material Sources and Sedimentary Environment of Gongchangling Iron Deposit. Mineral Deposits, 32, 380-396.
[8]
Bekker, A., Slack, J.F., Planavsky, N., Krapez, B., Hofmann, A., Konhauser, K.O. and Rouxel, O.J. (2010) Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic and Biospheric Processes. Economic Geology, 105, 467-508.
http://dx.doi.org/10.2113/gsecongeo.105.3.467
[9]
Gross, G.A. (1980) A Classification of Iron Formations Based on Depositional Environments. Canadian Mineralogist, 18, 215-222.
[10]
Zhai, M.G. and Santosh, M. (2011) The Early Precambrian Odyssey of North China Craton: A Synoptic Overview. Gondwana Research, 20, 6-25.
http://dx.doi.org/10.1016/j.gr.2011.02.005
[11]
Zhou, S.T. (1994) The BIF Geology of Anshan—Benxi Area. Geological Publishing House, Beijing.
[12]
Wan, Y.S., Dong, C.Y., Xie, H.Q., Wang, S.J., Song, M.C., Xu, Z.Y., Wang, S.Y., Zhou, H.Y., Ma, M.Z. and Liu, D.Y. (2012) Formation Ages of Early Precambrian BIFs in the North China Craton: SHRIMP Zircon U-Pb Dating. Acta Geologica Sinica, 86, 1447-1478.
[13]
Zhang, A.M., Wang, Y.J., Fan, W.M., Zhang, Y.Z. and Yang, J. (2012) Earliest Neoproterozoic (ca. 1.0 Ga) Arc-Back- Arc Basin Nature along the Northern Yunkai Domain of the Cathaysia Block: Geochronological and Geochemical Evidence from the Metabasite. Precambrian Research, 220-221, 217-233.
http://dx.doi.org/10.1016/j.precamres.2012.08.003
[14]
Middlemost, E.A.K. (1994) Naming Materials in the Mag-ma/Igneous Rock System. Earth Science Reviews, 37, 215- 224.
http://dx.doi.org/10.1016/0012-8252(94)90029-9
[15]
Sun, S.S. and McDonough, W.F. (1989) Chemical and Iso-topic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. In: Saunders, A.D. and Norry, M.J., Eds., Magmatism in Ocean Basins: Special Publication, Geological Society, London, 313-345.
http://dx.doi.org/10.1144/gsl.sp.1989.042.01.19
[16]
Shinjo, R. (1998) Petrochemistry and Tectonic Significance of the Emerged Late Cenozic Basalts behind the Okinawa Trough Ryukyu Arc System. Journal of Volcanology and Geothermal Research, 80, 39-53.
http://dx.doi.org/10.1016/S0377-0273(97)00042-5
[17]
Pearce, J.A. and Cann, J.R. (1973) Tectonic Setting of Basic Volcanic Rocks Determined Using Trace Element Analyses. Earth and Planetary Science Letters, 19, 290-300.
http://dx.doi.org/10.1016/0012-821X(73)90129-5
[18]
Shuto, K., Ishimoto, H., Hirahara, Y., Sato, M., Matsui, K., Fujibayanshi, N., Takazawa, E., Yabuki, K., Sekine, M., Kato, M. and Rezanov, A.I. (2006) Geochemical Secular Variation of Magma Source during Early to Middle Miocene Time in the Niigata Area, NE Japen: Asthenosphere Mantle Upwelling during Back-Arc Basin Opening. Lithos, 86, 1-33.
http://dx.doi.org/10.1016/j.lithos.2005.06.001
[19]
Cabanis, B. and Lecolle, M. (1989) Le diagramme La/10-Y/15-Nb/8: Un outil pour la discrimination des series volcaniques et lamise en evidence des processus demelange et/ou de contamination crustale. Compte Rendus de I’Académie des Sciences Series II, 309, 2023-2029.
[20]
Ghazi, J.M., Moazzen, M., Rahgoshay, M. and Moghadam, H.S. (2012) Geochemical Characteristics of Basaltic Rocks from the Nain Ophiolite (Central Iran); Constraints on Mantle Wedge Source Evolution in an Oceanic Back-Arc Basin and a Geodynamical Model. Tectonophysics, 574-575, 92-104.
http://dx.doi.org/10.1016/j.tecto.2011.10.001
[21]
Xu, J.F., Castillo, P.R., Chen, F.R., Niu, H.C., Yu, X.Y. and Zhen, Z.P. (2003) Geochemistry of Late Paleozoic Mafic Igneous Rocks from the Kuerti Area, Xinjiang, Northwest China: Implications for Back-Arc Mantle Evolution. Chemical Geology, 193, 137-154.
http://dx.doi.org/10.1016/S0009-2541(02)00265-6
[22]
Pearce, J.A. and Stern, R.J. (2006) Origin of Back-Arc Basin Magmas: Trace Element and Isotope Perspectives. In: Christie, D.M., Fisher, C.R., Lee, S.M. and Givens, S., Eds., Back-Arc Spreading Systems; Geological, Biological, Chemical, and Physical Interactions. Geophysical Monograph Series 166, American Geophysical Union, Washington, 63-86.
http://dx.doi.org/10.1029/166gm06
[23]
Münker, C. (1998) Nb/Ta Fraction in a Cambrian Arc-Back System, New Zealand: Source Constraints and Application of Refined ICPMS Techniques. Chemical Geology, 144, 23-45.
http://dx.doi.org/10.1016/S0009-2541(97)00105-8
