参考文献/References:
[1] Kametaka M, Takebe M, Nagai H, et al. Sedimentary environments of the Middle Permian phosphorite-chert complex from the northeastern Yangtze platform,China; the Gufeng Formation:a continental shelf radiolarian chert[J].Sedimentary Geology, 2005,174(3/4): 197-222.
[2] 田云涛,冯庆来,李琴.桂西南柳桥地区上二叠统大隆组层状硅质岩成因和沉积环境[J].沉积学报,2007,25(5):671-677.
[3] 杨水源,姚静.安徽巢湖平顶山中二叠统孤峰组硅质岩的地球化学特征及成因[J].高校地质学报, 2008,14(1):39-48.
[4] 刘新宇,颜佳新.华南地区二叠纪栖霞组燧石结核成因研究及其地质意义[J].沉积学报,2007,25(5):730-736.
[5] 周延. 江西华齐铜多金属矿区含矿硅质岩的地球化学特征及成因探讨[J].资源调查与环境,2011,32(1):57-65.
[6] 周永章,何俊国,杨志军,等.华南热水沉积硅质岩建造及其成矿效应[J].地学前缘,2004,11(2):373-377.
[7] 邱振,王清晨.广西来宾中上二叠统硅质岩海底热液成因的地球化学证据[J].中国科学:地球科学, 2011,41(5):725-737.
[8] 杨玉卿,冯增昭.华南下二叠统层状硅岩的形成及意义[J].岩石学报,1997,13(1):111-120.
[9] 王忠诚,吴浩若,邝国敦.广西晚古生代硅岩的地球化学及其形成的大地构造环境[J].岩石学报, 1995,11(4):449-455.
[10] Ledevin M, Arndt N T, Simionovici A. Archean cherts: field,petrographic and geochemical criteria to determine their origin[C].EGU General Assembly, 2013,15:4840.
[11] Marshall A O, Jehli(ˇoverc)ka J,Rouzaud J N, et al. Multiple generations of carbonaceous material deposited in Apex chert by basin-scale pervasive hydrothermal fluid flow[J].Gondwana Research, 2014,25(1):284-289.
[12] Kurihara T,Tsukada K,Otoh S, et al. Upper Silurian and Devonian pelagic deep-water radiolarian chert from the Khangai-Khentei belt of Central Mongolia:evidence for middle Paleozoic subduction-accretion activity in the central Asian orogenic belt[J]. Journal of Asian Earth Sciences, 2009,34(2):209-225.
[13] Baldwin G J,Thurston P C,Kamber R S. High-precision rare earth element,nickel,and chromium chemistry of chert microbands pre-screened with in-situ analysis[J].Chemical Geology, 2011,285(1):133-143.
[14] Nishikane Y,Kaiho K,Henderson C M, et al. Guadalupian-Lopingian conodont and carbon isotope stratigraphies of a deep chert sequence in Japan[J].Palaeogeography, Palaeoclimatology,Palaeoecology,2014, 403(2): 16-29.
[15] 周永章,涂光帜, Edward H,等.粤西古水剖面震旦系顶部层状硅质岩的热水成因属性:岩石学和地球化学证据[J].沉积学报,1994,12(3):1-11.
[16] 周永章.丹池盆地热水成因硅岩的沉积地球化学特征[J].沉积学报,1990,8(3):75-83.
[17] 李胜荣,高振敏.华南下寒武统黑色岩系中的热水成因硅质岩[J].矿物学报,1996(4):416-422.
[18] 张宁,夏文臣.华南晚古生代硅质岩时空分布及再扩张残留海槽演化[J].地球科学:中国地质大学学报, 1998,23(5):480-486.
[19] 夏萍,张湖,王秀璋,等.粤西长坑金银矿区硅质岩的地质地球化学特征及成因探讨[J].地球化学, 1996(2):129-139.
[20] 孙建东,骆学全,张雪辉,等.江西省铅山县二叠纪海相火山岩锆石U-Pb年龄及Lu-Hf同位素组成[J].华东地质,2016,37(4):246-251.
[21] 毛建仁,陶奎元,谢芳贵,等.闽西南地区成岩成矿作用与构造环境[J].岩石矿物学杂志, 2001,20(3):329-336.
[22] 王果胜,马文璞,朱卫平.闽西南晚古生代—早三叠世沉积特征及其大地构造意义[J].成都理工大学学报:自然科学版, 2009,36(1):87-91.
[23] 王森,张达,吕良冀,等.闽西南晚古生代以来伸展构造演化:中基性岩墙群的年代学、地球化学制约[J].大地构造与成矿学, 2015,39(5): 889-902.
[24] 王尔康,刘聪.闽西南—粤东北晚古生代的火山作用[M]北京:冶金工业出版社, 1993:178-186.
[25] 张达,吴淦国,狄永军,等.闽西南中生代推覆构造对铁矿床控矿特征研究[J].矿物学报,2011(Z):128-129.
[26] 周珍琦.闽西南地区推覆构造特征[J].石油实验地质,2006,28(1):38-41.
[27] Adachi M,Yamamoto K,Sugisaki R. Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication of ocean ridge activity[J].Sedimentary Geology, 1986,47(1/2):125-148.
[28] Yamamoto K. Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and Shimanto terrances[J]. Sedimentary Geology,1987,52(1/2):65-108.
[29] Murray R W. Chemical criteria to identify the depositional environment of chert:general priciples and applications[J].Sedimentary Geology, 1994,90(3/4):213-232.
[30] 路远发.Geokit:一个用VBA构建的地球化学工具软件包[J].地球化学,2004,33(5):459-464.
[31] Baltuck M. Provenance and distribution of tethyan pelagic and hemipelagic siliceous sediments, pindos mountains,Greece[J]. Sedimentary Geology, 1982,31(1):63-88.
[32] Murray R W, Ten Brink M R B, Gerlach D C, et al. Rare earth,major, and trace elements in chert from the Franciscan complex and Monterey Group,California: Assessing REE sources to fine-grained marine sediments[J].Geochimica et Cosmochimica Acta,1991,55(7):1875-1895.
[33] Murray R W, Buchholtz M, Jones D, et al. Rare earth elements as indicators of different marine depositional environments in chert and shale[J].Geology, 1990,18(3): 268-271.
[34] 燕长海,彭翼,刘国印,等.东秦岭二郎坪群热水沉积硅质岩的地球化学特征[J].地质通报, 2007,26(5):560-566.
[35] Michard A.Rare earth element systematics in hydrothermal fluids[J].Geochimica et Cosmochimica Acta, 1989,53(3):745-750.
[36] German C R, Klinkhammer G P, Edmond J M, et al. Hydrothermal scavening of rare earth elements in the ocean[J].Nature,1990,345(6275):516-518.
[37] Chen D Z, Qing H,Yan X, et al. Hydrothermal venting and basin evolution(Devonian, south China): Constraints from rare element geochemistry of chert[J]. Sedimentary Geology, 2006,183(3): 203-216.
[38] 福建地质矿产勘查局.福建省区域地质志[M].北京:地质出版社,1985.