Journal of Guangxi Normal University(Natural Science Edition) ›› 2012, Vol. 30 ›› Issue (1): 115-124.
ZHOU Ke-fa1,2, SUN Bao-sheng3, WANG Jin-lin2, ZHANG Nan-nan2, ZHANG Hai-bo2, WANG Wei2, LIAO Shi-bin2
CLC Number:
[1] 殷宝祥.新疆尉犁县且干布拉克蛭石矿床成因及矿床成因模式探讨[J].新疆地质,1992,10(1):6-22. [2] 高振家,陈晋,陆松年.新疆北部前寒武系[M].北京:地质出版社,1993:56-68. [3] 胡霭琴,张国新.新疆北部同位素地球化学研究新进展[J].矿物岩石地球化学通报,1991(3):171-173. [4] 胡霭琴,王中刚,涂光炽.新疆北部地质演化及成岩成矿规律[M].北京:科学出版社,1997:81-89. [5] 胡霭琴,张国新,陈义兵,等.新疆大陆基地分区模式和主要地质事件的划分[J].新疆地质,2001,19(1):12-20. [6] 成守德,徐新.新疆及邻近大地构造编图研究[J].新疆地质,2001,19(1):33-37. [7] HU Ai-qin,ROGERS G.Discovery of 3.3 Ga archaean rocks in northTarim Black of Xinjiang,Western China[J].Chinese Science Bulletin,1992(18):1546-1549. [8] LONG Xiao-ping,YUAN Chao,SUN Min,et al.Archean crustal evolution of the northern tarim craton,NW China:Zircon U-Pb and Hf isotopic constraints[J].Precambrian Research,2010,180:272-284. [9] LONG Xiao-ping,YUAN Chao,SUN Min,et al.The discovery of the oldest rocksin the Kuluketage area and its geological implications[J].Science China:EarthSciences,2011,54:342-348. [10] 郭召杰,张志诚,王建君.阿尔金山北缘蛇绿岩带的Sm-Nd等时线年龄及其大地构造意义[J].科学通报,1998,43(18):1981-1984. [11] 邹天人.新疆塔里木北缘碱性岩及成矿作用[J].矿床地质,1998,17(S1):71-72. [12] 邹天人,曹亚文,徐钰,等.塔里木盆地北缘新生代碱性玄武岩的地质地球化学[J].地质论评,1999,48(S1):1072-1077. [13] WILLIAM A B.The origin of the vermiculite deposit montana[J].The American Mineralogist,1959,44:282-299. [14] KULP J L.Notes on the dunite and the geochamistry of vermiculiteat the day book dunite deposit,Yancey County,North Carolina[J].Economical Geology,1954,49(2):1-14. [15] MITCHELL A H C,CARSON M S.Meneral deposit and global tectonic settings[M].London:Academic Press,1981:28-86. [16] VERHULST A,BALAGANSKAYA E,KIRNARSKY,et al.Petrological and geochemical (trace elements and Sr-Nd isotopes) characteristics of the PaleozoicKovdor ultramafic,alkaline and carbonatite intrusion (Kola Penisula,NW Russia)[J].LITHOS,2000,51(1-2):1-26. [17] CULLERS R L,GRAF J L.Rare earth elements in igneous rocks of the continental crust:predominantly basic and ultrabesic rocks[C]//HENDERSON P.Rare Earth Elements,Geochemistry.Amsterdam:Elsevier Science,1980,44(11):137-274. [18] 孙宝生,黄建华.新疆且干布拉克超基性岩-碳酸岩杂岩体Sm-Nd同位素年龄及其地质意义[J].岩石学报,2007,23(7):1611-1616. [19] VILADKAR S G,SUBRAMANNIAN V.Mineralogy and geochemisty of the carbonatitees of the Sevathur and Sam-alpatti Complexes,Tamil Nadu[J].JournalGeological Society of India,1995,45:505-517. [20] SUN Sen-san,McDONOUGH W F.Chemical and isotopic systematics ofoceanic basalts:implication for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345 [21] 李昌年.利用多阳离子参数解释花岗岩成因[J].基础地质译丛,1986,4:36-45. [22] 沈渭洲,方一亭,倪琦生,等.中国东部寒武系与奥陶系界线地层的碳氧同位素研究[J].沉积学报,1997,15(4):38-42. [23] 陈国耀.尉犁蛭石矿床的地质特征及成因探讨[J].新疆地质,1989,7(1):1-14. [24] 陶维屏,高锡芬,孙祁,等.中国非金属成矿系列[M].北京:地质出版社,1994:105-117. [25] MERTZ D F,DEVEY C W,TODT W,et al.Sr-Nd-Pb isotope evidenceagainst plume-asthenosphere mixing north of Iceland[J].Earth Planet Sci Lett,1991,107:243-255. [26] THONI M,JAGOUTZ E.Some new aspects of dating ecologites inorogenic belts:Sm-Nd,Rb-Sr and Pb-Pb isotopic results from the Austroalpine Saualpe and Koralpe type-locality[J].Geochim Cosmochim Acta,1992,56:347-368. [27] SAN B S,HUANG J L.Sm-Nd isotopic age of Qieganbulak ultrabasic-carbonafite complex in Xinjiang,China and its geological significance[J].Acta Petrologica Sinica,2007,23(7):1611-1616. [28] HOEFS J.Stable isotope geochemistry[M].Berlin:Springer,1987:30-90. [29] 杜天乐.地壳流体与地幔流体间的关系[J].地学前缘,1996,3(3/4):172-180. [30] ANDERSON D L.Hotspots,basalts and the evolution of the mantle[J].Science,1981,213:82-89. [31] 陶维屏.关于超大型非金属矿床研究问题[J].中国非金属矿业导刊,1996(3):2-8. |
No related articles found! |
|