Anderson A T. 1984. Probable relation between plagioclase zcning and magma dynamics, Fuego Volcano, Guatemala. Am. Mineral.,69: 660～670.
[13]
Arculus R J, Will K J. 1980. The petrology of igneous blocks and inclusions from the Lesser Antilles island, eastern Aleu:ian arc,Alaska. J. Geol. , 85: 177～186.
[14]
Bartels K S, Kinzler R J, Grove T L. 1991. High pressure phase relations of primitive high-alumina basalts from Medicine Lake volcano, northern California. Contrib. Mineral. Petrol. , 108: 253～270.
[15]
Brophy J D. 1986. The Cold Bay volcanic center, Aleutian volcanic arc: Implications for the origin of hi alumina arc basalt. Contrib.Mineral. Petrol., 93:368～380.
[16]
Chen Rong, Zhou Jincheng. 1999. Information of crust-mantle interaction implied in early Cretaceous composite lavas and dikes from eastern Zhejiang. Geological Review, 45 (Sup.): 784～ 795(in Chinese with English abstract).
[17]
Feng Zongzhi, Bian Runzhang,Huang Shuixing,et al. 1991. Mesozoic volcanology and mineralization related to volcanics in YongtaiDehua district, Fujian province. Bulletin of the Nanjing instituteof geology and mineral resources, Chinese Academy of Geological Sciences, Supplement, 9:1 ～ 100 ( in Chinese with English abstract).
[18]
Kuno H. 1950. Petrology of Hakone volcano and the adjacent areas, Japan. Geol. Soc. Am. Bull. , 61: 957～1020.
[19]
Kuno H. 1960. High-alumina basalt. J. Petrol. , 1: 12～145.
[20]
Leake B E. 1978. Nomenclature of amphiboles. Can. Mineral. , 16:636～651.
[21]
Li Huimin, Dong Chuanwan, Xu Xisheng, Zhou Xinmin. 1995.Dating of U-Pb by single zircon from Quanzhou gabbro-crigin of basic igneous rocks from southeastern Fujian. Chinese Science Bulletin, 40(2): 158～160 ( in Chinese ).
[22]
Li Xianhua, Hu Ruizhong, Rao Bing. 1997. Geochronology and geochemistry of Cretaceous mafic dikes from northern Guangdong, SE China. Geochimica, 26 (2): 14 ～ 31 ( in Chinese with English abstract).
[23]
Marsh B D. 1982. The Aleutian. In: Thorpe R S, ed. Andesites.Wiley. 99 ～ 114.
[24]
Myers J D, Marsh B D, Sinha A K. 1986. Geochemical and strontium isotopic characteristics of parental Aleutian arc magmas: evidence from the basaltic lavas of Atka. Contrib. Mineral. Petrol. , 94:1～11.
[25]
Panjasawatwong Y, Danyushevsky L V, Crawford A J, Harris K L. 1995. An experimental study of the effects of melt composition on plagioclase-melt equilibria at 5 and 10 kbar: implication for the origin of magmatic high-An plagioclase. Contrib. Mineral.Petrol., 118: 420～432.
[26]
Sis son T W, Grove T L. 1993a. Temperatures and H2O contents of low-MgO high-alumina basalts. Contrib. Mineral. Petrol. , 113:167～184.
[27]
Sisson T W. Grove T L. 1993b. Experimental investigations of the role of H2O in calc alkaline differentiation and subduction zone magmatism. Contrib. Mineral. Petrol. , 113: 143～ 166.
[28]
Sis son T W, Grove T L, Coleman D S. 1996. Hornblende gabbro sill complex at Onion Valley, California, and a mixing origin for the Sierra Nevada batholith. Contrib. Mineral. Petrol., 126:81～108.
[29]
Wang Dezi. Zhou Jincheng, Qiu Jiansheng, Zhang Haijin. 1994. The magma mixing in early Cretaceous volcanic activities and evidence for crust mantle interaction in southeastern coast of China. Journal of Nanjing University (Earth Sciences) : 6(4) : 317～325(in Chinese with English abstract).
[30]
Wang Zhihong, Lu Huafu. 1999. Sm-Nd isochron age of the cumulate gabbro from the Fujian coastal region,southeastern China and itm implication. Geological Review, 45 (4): 408 ～ 410 (in Chinese with English abstract).
[31]
Wilson M. 1989. Igneous Petrogenesis. Published by Chapman &. Hall, 2～6 boundary Row, London SE1 8HN, UK.
[32]
Yang Zhuliang, Shen Wezhou, Tao Kuiyuan, Shen Jialin. 1999. Sr,Nd and Pb isotopic charateristics of early Cretaceous basaltic rocks from the coast of Zhejiang and Fujian: evidence for ncientenriched mantle source . Scientia Geologica Sinica, 34 (1): 59～67 (in Chinese with English abstract).
[33]
Yu Yunwen, Zhou Taixi, Chen Jiangfeng. 1993. The characteristics and origin of the Xuantandi bimodal volcanic rocks of the late stage of early Cretaceous,Zhejiang. Journal of Nanjing University (Earth Sciences),5(4):420～429 (in Chinese with English abstract).
[34]
Yoder H S Jr. 1969. Calcalkalic andesites: experimental evidence bearing on the origin of their assumed characteristics. In:McBirner A R ,ed. Proc Andesite Conf. Oregon Dept of Geol and Mineral Industries, Bull., 65: 77～89.
Dong Chuanwan, Xu Xisheng , Chen Xiaoming , Zhou Xinmin. 1997. Mineralogical record of crystallization processes of Pingtan horblande gabbro, Fujian. Acta Mineralogica Sinica, 17(3): 285 ～290 (in Chinese with English abstract).
[37]
Dong Chuanwan, Li Wuxian, Xu Xisheng, Zhou Xinmin. 1998. Late Mesozoic magma mixing in southeastern Fujian: petrologic evidence of igneous comples from Pingtan . Progress in Natural Science, 8(5): 581～586 (in Chinese ).
[38]
Pitcher W S, Atherton M P, Cobbing E J, Beckinsale R D, ed. 1985.Magmatism at a plate edge: the Peruvian Andes. Wiley, New York.
[39]
Singer B S, Myers J D, Frost C D. 1992. Mid Pleistocene lavas from the Seguam volcanic center, central Aleutian arc: closed-system fractional crystallization of a basalt to rhyodacite eruptive suite. Contrib. Mineral. Petrol., 110: 87～117.
Zhou Xinmin, Xu Xisheng, Dong Chuanwan, Li Huimin. 1994.Mineralogical mark of active continental margin of southeastern China: anorthitic plagioclase. Chinese Science Bulletin , 39 (11):1011 ～ 1014 (in Chinese).
