1 Dodd RT, Jarosewich E (1979): Incipient melting in and shock classification of L-group chondrites. Earth Planet Science Letter, 44: 335-340. DOI:10.1016/0012-821X(79)90181-X 2 Stöffler D, Keil K, Scott ERD(1991): Shock metamorphism of ordinary chondritis. Geochimicaet Cos-mochimica Acta, 55: 3845-3867. DOI:10.1016/0016-7037(91)90078-J 3 Chen M, Sharp TG, ElGoresy A et al. (1996): The majoritepyrope + magnesiowüstite assemblage: constraints on the history of shock veins in chondritis. Science, 271: 1570-1573. DOI:10.1126/science.271.5255.1570 4 Gillet P, Chen M, Dubrovinsky L et al. (2000): Natural NaAlSiO hollandite in the shocked Six iang kou meteorite. Science, 287: 1633-1636. 3 8 DOI:10.1126/science.287.5458.1633 5 Xie Z, Sharp TG, De Car li PS(2006): High-pressure phases in shock-induced melt veins of the Ten ham L6 chondrite: Constraints of shock pressure and duration. Geochemicaet Cosmochimica Acta, 70: 504-515. DOI:10.1016/j.gca.2005.09.003 6 Rubin AE, Scott ERD, Keil K (1997): Shock metamorphism of enstatite chondrites. Geochimicaet Cosmochimica Acta, 61(12): 847-858. 7 Xie X, Chen M, Wang D(2001): Shock-related mineralogical features and PT history of the Suizhou L5 chondrite. European Journal of Mineralogy, 13: 1177-1190. DOI:10.1127/0935-1221/2001/0013-1177 8 Katsura T, Yamada H, Nishikawa O et al. (2004): Olivine-wadsleyite transition in the system (Mg, Fe)SiO. Jounal of Geophysics Research, 109: B02209. 2 4 9 Inoue T, Irifune T, Higo Y et al. (2006): The phase boundary between wadsleyite and ringwoodite in MgSiO determined by in situ Xray diffraction. Phys Chem Minerals, 33: 106-114. 2 4 DOI:10.1007/s00269-005-0053-y 10 Mcmillan P, Akaogi M (1987): Ram an spectra of MgSiO (modified spinel) and MgSiO (spinel). American Mineralogist, 72: 361-364. 2 4 2 4 11 Malavergne VGF, Benzerara K, Martinez I(2001): Description of new shock-induced phases in the Shergotty, Zagami, Nakhla, and Chassigny meteorites. Meteoritics & Planetary Science, 36: 1297-1350. 12 Tomiokab N, Kmiura M (2003): The breakdown of diopside to Ca-rich majorite and glass in a shocked H chondrite. Earth and Planetary Science Letters, 208: 271-278. DOI:10.1016/S0012-821X(03)00049-9 13 Chen M, Xie X, ElGoresy A(2004): A shock-produced (Mg, Fe) SiO glass in the Suizhou meteorite. Meteoritics & Planetary Science, 39: 1797-1808. 3 14 Trukhin ACB(2005): Ram an and optical reflection spectra of germanate and silicate glasses. Journal of Non Crystalline Solids, 351: 3640-3643. DOI:10.1016/j.jnoncrysol.2005.09.017 15 Yagi A, Suzuki T, Akaogi M (1994): High pressure transitions in the system KAlSiO-NaAlSiO. Physics and Chemistry of Minerals, 21: 12-17. 3 8 3 8 16 Tutti F(2007): For mation of end member NaAlSiO holl and ite-type structure (lingunite) in diamond anvilcell. Physics of The Earth and Planetary Interiors, 161(3-4): 143-149. 3 8 DOI:10.1016/j.pepi.2007.02.004 17 Xie XD, Chen M, Wang DQ et al. (2006): Melting and vitrification of plagioclase under dynamic high pressures. A cta Petrologica Sinica, 022: 503-509. 18 Chen M, El Goresy A(2000): The nature of maskelynite in shocked meteorites: not a diaplectic glass but a glass from shock-induced dense melt at high pressure. Earth and Planetary Science Letters, 179: 485-502. 19 Agee CB, Li J, Shannon MC et al. (1995): Presure-tem perature phase diagram for the Allen demeteorite. Jounal of Geophysics Research, 100: 17725-17740. DOI:10.1029/95JB00049