Rapp R P and Watson E B. 1995. Dehydration melting of metabasalt at 8-32 kbar: implications for continental growth and crust-mantle recycling. J Petrol, 36: 891-931.
[2]
Sajona F G, Bellon H, Maury R C Pubellier M, Cotton J and Rangin C. 1994. Magmatic response to abrupt changes in geodynamic settings: Pliocene-Quaternary calc-alkaline and Nb-enriched lavas from Mindanao (Philippines). Tectonophysics, 237: 47-72.
[3]
Sajona F G, Maury R C, Bellon H, Cotton I J, Defant M J and Pubellier M. 1993. Initiation of subduction and the generation of slab melts in western and eastern Mindano, Philippines. Geology, 21: 1007-1010.
[4]
Sajona F G, Naury R C, Pubellier M, Leterrier J, Bellon H and Cotton J. 2000. Magmatic source enrichment by slab-derived melts in a young post-collision setting, central Mindanao(Philippines). 54: 173-206.
[5]
Sheppard S, Griffin T J, Tyler I M and Page R W. 2001. High- and low-K granites and adakites at a Paleoproterozoic plate boundary in northwestern Australia. J Geol Soc London, 158: 547-560.
[6]
Stern C R and Kilian R. 1996. Role of the subducted slab, mantle wedge and continental crust in the generation of adakites from the Andean Austral Volcanic Zone. Contri Mineral Petrol, 123: 263-281.
[7]
Turner S, Arnaud N, Liu J, Rogers, Hawkesworth C, Harris N, Kelley S, Van calsteren P and Deng W. 1996. Post-collision, shoshonitic volcanism on the Tibetan Plateau: implications for convective thinning of the lithosphere and the source of ocean island basalts. J Petrology, 37: 45-71.
[8]
Wang Q, Xu J, Wang J, Zhao Z, Qiu J, Wang R, Xiong X,Sang L and Peng L. 2000. The recognization of adakite-type gneisses in the North Dabie Mountains and its implication to ultrahigh pressure metamorphic geology. Chinese Science Bulletin, 45: 1927-1933.
[9]
Wang Q, Zhao Z H, Xiong X L and Xu J F. 2001. Melting of the underplating basaltic lower crust: evidence from the Shaxi adakitic sodic quartz diorite-porphyrites, Anhui Province, China. Geochimica, 30: 353-362.
[10]
Wu F Y, Ge W C and Sun D Y. 2002. The definition, diacrimination of adakites and their geological role. In: Xiao Q H, Deng J F, Ma D Q et al., eds. The Ways of Investigation on Granitoids. Beijing: Geological Publishing House, 172-191.
[11]
Xiong X L, Zhao Z H, Bai Z H, Mei H J, Wang Y X, Wang Q, Xu J F and Bao Z W. 2001. Adakite-type sodium-rich rocks in Awulale Mountain of west Tianshan: Significance for the vertical grown of continental crust. Chinese Science Bulletin, 46: 811-817.
[12]
Zhang Q, Qian Q, Erchie W. Wang Y, Zhao T P, Hao J and Guo G J. 2001. Existance of East China Plateau in mid-late Yanshan period: implication from adakites. Scientia Geologica Sinica, 36: 248-255 (in Chinese with English abstract).
[13]
Zhang Q, Wang Y, Qian Q, Yang J H, Wang Y L and Zhao T P. 2001. The chatacteristics and tectonic-metallogenic signifances of the Mesozoic adakites in eastern China. Acta Petrol Sinica, 17: 236-244 (in Chinese with English abstract).
Defant M J and Drummond M S. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347: 662-665.
[16]
Edwards S J. 1995. Boninitic and tholeiitic dykes in the Lewis Hills mantle section of the Bay of Islands Ophiolite; implications for magmatism adjacent to a fracture zone in a back-arc spreading environment. Can J Earth Sci, 32: 2128－2146.
[17]
Feeley T C and Hacker M D. 1995. Intracrustal derivation of Na-rich andesitic and daitic magmas: an example from Volcan Olague, Andean Central Volcanic Zone. The Jounal of Geology, 103: 213-225.
[18]
Ge X Y, Li X H, Chen Z G and Li W P. 2002. Geochemistry and petrogenesis of Jurassic high Sr/low Y granitoids in eastern China: Constrains on crustal thickness. Chinese Science Bulletin, 47: 962-968.
[19]
Gibb F G F and Kanaris-Sotiriou R. 1988. The geochemistry and origin of the Faeroe-Shetland sill complex. In: Morton A C, eds. Early Tertiary Volcanism and the Opening of the NE Atlantic. London: Geol. Soc. Blackwell Publ. (39): 241～252.
[20]
Kay R W. 1978. Aleutian magnesian andesites: melts from subducted Pacific ocean crust. J Volcanol Geothermal Res, 4: 497-522.
[21]
Li Wuping,Li Xianhua and Lu Fengxiang. 2001. Genesis and geological significance for the middle Jurassic High Sr and lower Y type volcanic rocks in Fuxin area of West Liaoning, northeastern China. Acta Petrologica Sinica, 17: 523-532.
[22]
Peacock S M, Rushmer T and Thompson A B. 1994. Partial melting of subducting oceanic crust. Earth Planet Sci Lett, 121: 227-244.
[23]
Petford N and Atherton M. 1996. Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru. J Petrol, 37: 1491－1521.
[24]
Rapp R P, Xiao L and Shimizu N. 2002. Experimental constraints on the origin of potassium-rich adakites in eastern China. Acta Petrologica Sinica, 18: 293-302.
Atheton M P and Petford N. 1993. Generation of sodium-rich magmas from newly underplated basaltic crust. Nature, 362: 144-146.
[37]
Bedard J H, Lauziere K, Tremblay A and Sangster A. 1998. Evidence for forearc seafloor-spreading from the Betts Cove ophiolite,Newfoundland: oceanic crust of boninitic affinity. Tectonophysics, 284: 233-245
[38]
Castillo P R, Janney P E and Solidum R U. 1999. Petrology and geochemistry of Camiguin island, southern Philippines: insights to the source of adakites and other lavas in a complex arc setting. Contrib Mineral Petrol , 134: 33-51.
[39]
Castillo P R. 2002. The origin of some of the adakite-like and Nb-enriched lavas in southern Philippines. Acta Petrologica Sinica, 18: 143-151..
[40]
Chen B, Jahn B M and Wei C J. 2002. Petrogenesis of Mesozoic granitoids in the Dabie UHP complex, Central China: trace element and Nd-Sr isotope evidence. Lithos, 60: 67－88
[41]
Chen Y X and Chen W J. 1997. Mesozoic volcanic rocks in western Liaoning Province and surrounding area-geochronology, geochemistry and tectonic environment. Beijing: Seis. Publ. House, 1-279(in Chinese).
[42]
Crawn A J, Falloon T J and Green D H. 1989. Classification, petrogenesis and tectonic settings of boninites. in: Crawford A J. ed. Boninite, London: Unwin Hyman, 1－49.
[43]
Defant M J. 2002. Reply for comment by R. Conner on the "Evidence suggests slab melting in arc magmas" by M Defant and P Kepezhinskas (EOS, 2001, 82: 65, 68-69). EOS, 66: 256-257.
[44]
Defant M J, Xu J F, Kepezhinskas P, Wang Q, Zhang Q and Xiao L. 2002. Adakites: some variations on a theme. Acta Petrologica Sinica, 18: 129-142.
[45]
Drummond M S, Defant M J and Kepezhinskas P K. 1996. Petrogenesis of slab derived trondhjemite -tonalite-dacite/adakite magmas. Trans R Soc Edingburgh: Earth Sci, 87: 205-215.
[46]
Eby G N. 1992. Chemical subdivision of the A-type granitoids: Petrogenetic and implications. Geology, 20: 641-644.
[47]
Gutscher M A, Maury R, Eissen J and Bourdon E. 2000. Can slab melting be caused by flat subduction? Geology, 28: 535-538.
[48]
Harris N R, Sisson V B, Wright J E and Pavlis T L. 1996. Evidence for Eocene mafic underplating during fore-arc intrusive activity, eastern Chugach Mountains, Alaska. Geology, 24: 263-266.
[49]
Hickey R L and Frey F A. 1982. Geochemical characteristics of boninite series volcanics: implications for their source. Geochimica et Cosmochimica Acta, 46 : 2099-2115.
[50]
Kay R W and Kay S M. 2002. Andean adakites: three ways to make them. Acta Petrologica Sinica, 18: 303-311.
[51]
Kay S M and Mpodozis C. 2001. Central Andean ore deposits linker to evolving shallow subduction systems and thinkening crust. GSA Today, 4-9.
[52]
Loisell M C and Wones D K. 1979. Characteristics and origin of anorogenic granite. Geol Soc Am Abstr Program, 11: 468.
[53]
Ma C, Li Z, Ehlers C, Yang K and Wang R. 1998. A post-collisional magmatic plumbing system: Mesozoic granitoid plutons from the Dabieshan high-pressure and ultrahigh-pressure metamorphic zone, east-central China. Lithos, 45: 431－456.
[54]
Martin H. 1999. Adakitic magmas: modern analogues of Archean granitoids. Lithos, 46: 411-429.
[55]
Muir R J, Weaver S D, Bradshaw J D, Eby G N and Evans J A. 1995. The Cretaceous Separation Point batholith, New Zealand: granitoid magmas formed by melting of mafic lithosphere. J Geol Soc London, 152: 689-701.
[56]
Qian Q, Chung S L, Lee T Y and Wen D J. 2002. Geochemical characteristics and petrogenesis of the Badaling high Ba-Sr granitoids: a comparison of igneous rocks from North China and the Dabie-Sulu Orogen. Acta Petrologica Sinica, 18: 275-292.
[57]
Xiong X L, Zhao Z H, Bai Z H, Mei H J, Zhu J C and Rao B. 2001. Origin of Awulale adakitic sodium-rich rocks in western Tianshan: Constraints for Nd and Sr isotopic compositions. Acta Petrol Sinica, 17: 514-522 (in Chinese with English abstract).
[58]
Xu J F, Shinjo R, Defant M J, Wang Q and Robert P. 2002. Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Geology, 30: 1111-1114.
[59]
Yogodzinski G M, Kay R W, Volynets O N, Koloskov A V and Kay S M. 1995. Magnesian andesite in the western Aleutian Komandorsky region: implications for slab melting and pressures in the mantle wedge. Geol Soc Am Bull, 107: 505-519.
[60]
Yumul Jr, G P, Dimalanta C B, Bellon H, Faustino D V, De Jesus J V, Tamayo Jr R A and Jumawan F T. 2000. Adakitic lavas in the central Luzon back-arc region, Philippines: lower crust partial melting products? The Island Arc, 9: 499-512.
