当前位置: 首页> 范文大全> 辞职报告>

安徽南部溪口岩群流纹岩地球化学特征及成因

发布时间:2022-02-11 08:42:09 浏览数:

zoޛ)j馓 8&N#2sEZJ	
lkDA6]yuӡ.x_m=_;m5M]<uPiid|Ow!>AECD4A
4CD4A=vi]5ߙiәןwwiݤi]eb<Ĺ_}R{O;m�c~ם|׍5{Ӿ:ܭ~x]Z5ֶ;;NM5+cӭ5M;N6]C ;MtnК;MӞ 馔;d;mvM۽{4ymמNH=no0ݢ+(+vvQl)yC[=}8N-y~?M^x]t~]:-tDn}睷ۭ{߾<^k4KNӍĻ_8m_駏駍}MLWk:z8c}v^t8f4N/ٮ[ummo[~o[o[㝸Eo]|
:}t]uӣbnz]:MtnKk7n6X5#Ju^�#JuqoN#cf[a6}6aӇoiۭyu2^	d[J`PfN调查报告[R].黄山:安徽省地质矿产勘查局332地质队,1971.

[2] 中国地质调查局南京地质调查中心.1∶5万虹关幅、平里幅、江潭幅、瑶里幅区域地质调查报告[R].南京:中国地质调查局南京地质调查中心,2009.

[3] 张彦杰,周效华,廖圣兵,等.皖赣相邻鄣公山地区新元古代地壳组成及造山过程[J].地质学报,2010,84(10):1401-1427.

[4] 张彦杰,周效华,廖圣兵,等.江南造山带北缘鄣源基性岩地质—地球化学特征及成因机制[J].高校地质学报,2011,17(3):393-405.

[5] 高林志,张传恒,刘鹏举,等.华北—江南地区中、新元古代地层格架的再认识[J].地球学报,2009,30(4):433-446.

[6] 马荣生.皖南前南华纪岩石地层[J].资源调查与环境,2002,23(2):94-106.

[7] 廖圣兵,张彦杰,周效华,等.皖赣相邻地区溪口岩群沉积序列及沉积环境分析[J].矿产与地质,2014,28(6):660-667.

[8] 徐生发,朱强,胡召齐.皖南新元古代溪口岩群岩石地球化学特征及其构造意义[J].安徽地质,2017,27(1):1-6.

[9] 江来利,胡召齐,朱强,等.皖浙赣相邻区晚中生代多期构造变形特征及其动力学背景[J].地学前缘,2016,23(4):137-147.

[10]安徽省地质矿产勘查局,安徽省地质调查院.安徽省区域地质志[R].2014.

[11]李献华,刘颖,涂湘林,等.硅酸盐岩石化学组成的ICP-AES和ICP-MS准确测定:酸溶与碱熔分解样品方法的对比[J].地球化学,2002,31(3):289-294 .

[12]WILSON M.Igneous petrogenesis[M].London:Unwin Hyman Press,1989:295-323.

[13]LEBAS N J,LEMAITRE R W,STRECKEISEN A,et al. Chemical classification of volcanic rocks based on the total alkali- silica diagram[J].Journal of Petrology,1986,27(3):745-750.

[14]MANIAR P D,PICCOLI P M.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,1989,101(5):635-643.

[15]邱军强,彭智,陈芳,等.北淮阳东段杨家湾岩体地球化学特征、锆石U-Pb定年及地质意义[J].华东地质,2016,37(2):89-96.

[16]LIU Y J,CAO L M,LI Z L,et al.Element geochemistry[M].Beijing:Science Press,1984:50-372.

[17]熊兴国,岳龙,徐安全,等.西藏羌塘达尔应强过铝花岗岩地球化学特征及地球动力学意义[J].沉积与特提斯地质,2006,26(4):40-46.

[18]SUN S S,McDONOUNGH W F.Chemical and isotopic systematics of oceanic basalt:Implications for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345.

[19]SAJONA  F G,MAURY R C,BELLON H,et al.Initiation of subduction and the generation of slab melts in western and eastern Mindanao,Philippines[J].Geology,1993,21(11):1007-1010.

[20]ELIER J M,CRAWFORD  A,ELLIOTT T,et al.Oxygen isotope geochemistry of oceanic arc lavas[J].Journal of Petrology,2000,41(2):229-256.

[21]劉寿和,夏邦栋.皖南晚元古代火山岩及其构造背景[J].南京大学学报,1990(1):43-52.

[22]林强,葛文春,曹林,等.大兴安岭中生代双峰式火山岩的地球化学特征[J].地球化学,2003,32(3):208-222.

[23]刘俊杰,鞠文信,赵九峰,等.大兴安岭根河岩区晚侏罗世火山岩特征及构造环境探讨[J].华南地质与矿产,2006,22(1):38-46.

[24]HILDRETH  W,MOORBATH S.Crustal contributions to arc magmatism in the Andes of central Chile[J].Contributions to Mineralogy and Petrology,1988,98(4):455-489.

[25]邓晋福.岩石相平衡与岩石成因[M].武汉:武汉地质学院出版社,1987:58-67.

[26]薛怀民,马芳,宋永勤,等.江南造山带东段新元古代花岗岩组合的年代学和地球化学:对扬子与华夏地块拼合时间与过程的约束[J].岩石学报,2010,26(11):3215-3244.

[27]PEARCE J A,HARRIS N B W,TINDLE A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,1984,25(4):956-983.

Geochemical characteristics and petrogenesis of rhyolites ofthe Xikou Group in South Anhui Province

ZHAO Xian-chao,SUN Ming-ming,WU Li-bin,WANG Li-min

(Geological Survey of Anhui Province,Hefei 230001,China)

Abstract:Rhyolites of the Xikou Group are tectonically located at the southeastern part of the Yangtze Plate and the eastern Jiangnan Orogen, with outcrop mainly in the Xiuning area, South Anhui Province. This study investigated the petrogenesis and tectonic setting of Xikou Group rhyrolites through petrographic and geochemical analysis. Geochemical characteristics of major elements indicate that the rhyolites are characterized by high SiO2,high Na and low K,high Al2O3,low MgO,low CaO,low TiO2,and low MnO,suggesting a typical calc-alkaline series with peraluminous features. Geochemical characteristics of trace elements show that rhyrolites are eichment of large-ionlithophile elements K and Rb, relative depletion of Ba, Sr, Sm and Ce; obvious eichment of high field strength element U, relatively depletion of Nb, P, Zr and Hf, obviously depletion of Ti. The total REE content is (25.11~54.51)×10-6,with slightly eiched LREE, relatively depleted HREE and significant LREE-HREE differentiation. Chondrite-normalized REE distribution patterns show obviously right-dipping and distinct Eu negative anomaly. The above study suggests that the Xikou Group rhyolites in South Anhui were product of partial melting of the oceanic crust and formed in a volcanic arc tectonic environment related to syncollision.

Key words:Xikou Group;rhyolite;geochemical characteristics;petrogenesis;tectonic setting;South Anhui Province

上一篇:风景名胜区内的温泉存废之争

上一篇:监管变掠夺,监察大队长成大矿主

相关范文