[1] Winston D,Rittel John F,Funiss George.Gas bubble and expansion on molar-tooth calcite structures in the Middle Proterozoic Belt Supergroup Western Monrtana-Reply[J].Journal of Sedimentary Research,1999,69(5):1 140-1 145.
[2] Bauerman H. Report on the Geology of the Country Near the Forth-ninth Parallel of North Latitude West of the Rocky Mountains[Ｒ].Canada Geological  Survey of Report Progress 1882-1884,1885,partB:1-42. 
[3] James N P, Narbonne G M, Sherman A G.Molar tooth carbonates:Shallow subtidal facies of the Mid to Late Proterozoic[J].Journal of Sedimentary Research,1998,68(5):716-722.
[4] Ge Ming,Meng Xinghua,Kuang Hongwei, et al. Molar-tooth Carbonates:Carbonate research highlight of the world in the 21st century[J].Acta Sedimentologica Sinica,2003,21(1):81-89. [葛铭,孟祥化,旷红伟,等.微亮晶(臼齿)碳酸盐岩:21世纪全球地学研究的新热点[J].沉积学报,2003,21(1):81-89.]
[5] Qiao Xiufu, Song Tianrui,Gao Linzhi, et al. Seismic succession of oscillatory liquefaction in carbonate rocks[J].Acta Geologica Sinica,1994,68(1):16-34. [乔秀夫,宋天锐,高林志,等.碳酸盐岩振动液化地震序列[J]. 地质学报,1994,68 (1):16-34.]
[6] Qiao Xiufu, Ji Qiang, Gao Linzhi, et al. Stratigraphic correlation of the Sinian in the Eastern part of  the Northern China plate[J]. Regional Geology of China, 1996, (2):135-142. [乔秀夫,  季强,  高林志,等.  北中国板块震旦纪地层对比[J].  中国区域地质, 1996, (2):135-142.]
[7] Qiao Xiufu,Gao Linzhi. Neoproterozoic and early Pleozoic seismic disaster events in the North China platform and their relationship  with Rodonia[J].Chinese Science Bulletin,1999,44(16):1 753-1 757. [乔秀夫,高林志.华北中新元古代及早古生代地震灾变事件及与Rodinia的关系[J].科学通报,1999,44(16):1 753-1 757.]
[8] Qiao Xiufu,Gao Linzhi,Peng Yang.Neoproterozoic in Paleo-Tanlu Fault Zone[M]. Beijing:Geological Publishing House,2001. [乔秀夫,  高林志,  彭阳.  古郯庐带新元古界[M].北京:  地质出版社,2001.]
[9] Liu Yanxue,Kuang Hongwei,Cai Guoyin, et al.Depositional environments  of Molar-tooth limestones of the Neoproterozoic Yingchengzi Formation in southern Liaoning[J].Geological Bulletin of China,2003,22(6):419-425. [刘燕学,旷红伟,蔡国印,等.辽南新元古代营城子组臼齿灰岩的沉积环境[J].地质通报,2003,22(6):419-425.]
[10] Smith A G.  The origin and deformation of some“Molar-tooth”structure in the Precambrian Belt-Purcell supergroup[J].Journal of Geology,1968,76:426-433.
[11] Ricketts B D,Donaldson J A. Sedimentary history of the Belcher Group of Hudson Bay[A]. In:   Campbell F H A,ed. Proterozoic basin of Canada[C].Geology Survey of Canada,1981,81(10):235-254. 
[12] Shields G A.Working towards a new stratigraphic cabibration Scheme for the Neoproterozoic-Cambrian[J].  Eclogae Geologicae,Helvetiae,1999, 92:221-233.
[13] Shields G A.“Molar-tooth microspar”: A chemical explanation for its disappearance ~ 750 Ma[J]. Terra Nova, 2002,14: 108-113.
[14] Knoll A H. Microbiotas of the Late Precambrian Hunnberg formation, Nordaustlandet[J].Svalbard: Journal of Paleontology,1984,58:131-162.
[15] Kaufman A J,Knoll A H. Neoproterozoic variations in the C-isotopic composion of seawater: Stratigraphic and biogeochemical implications[J].Precambrian Research, 1995,73:27-49.
[16] Huang Sijing,Shi He,Liu Jie,et al. Progress in strontium isotope stratigraphy[J].Advances in Earth Science,2001,16(2):194-200.[黄思静,石和,刘洁,等.  锶同位素地层学研究进展[J].地球科学进展,2001,16(2):194-200.]
[17] Yang Jiedong,Zheng Wenwu,Wang Zongzhe,et al. Age determining of the Upper Precambrian  System of Northern Jiangsu-Anhui by using Sr and C isotopes[J].Journal of Stratigraphy, 2001,25(1):44-47. [杨杰东,郑文武,王宗哲,等.  Sr、C同位素对苏皖北部上前寒武系时代的界定[J].地层学杂志,2001,25(1):44-47.]
[18] Zheng Wenwu,Yang Jiedong,Hong Tianqiu,et al. Sr and C Isotopic correlation and the age boundary determination for the Neoproterozoic in the South Liaonan and Northern Jiangsu-Northern Anhui provinces[J].Geological Journal of China Universities,  2004,10(2):165-178. [郑文武,杨杰东,洪天求,等. 辽南与苏皖北部新元古代地层Sr和C同位素对比及年龄界定[J].高校地质学报, 2004,10(2):165-178.]
[19] O’Connor M P. Classification and environmental interpretation of the cryptalgal organosedimentary “Molar-tooth” structure from the late Precambrian Belt-Purcell Supergroup[J]. Journal of Geology,1972,80(５): 592-610.
[20] Horodyski R J. Sedimentary geology and stromolites of the Middle Proterozoic Belt Supergroup, Glacier National Park, Montana[J].Precambrian Research, 1983,20:391-425.
[21] Grozinger J P. Shallowing-upward cycles of the Wallace formation Belt Supergroup, northwestern Montana and adjacent areas[J].  Montana Bureau of Mines and Geology Special Publication,1986, 94:143-160.
[22] Winston D. Sedimentolgy of the Ravalli Group, middle Belt carbonate and Washington[A]. In: Roberts S M, ed.Belt Supergroup: Aguide to Proterozoic Rockw of Western Montana and Adjacent Areas[C].  Montana Bureau of Mines and Geology Special Publication ,1986, 94:245-257.
[23] Winston D A. sedimentology and tectonic interpretation of Belt[A]. In: Winston D, Horodyski R J, Whipple J W,eds. Middle Proterozoic Belt Supergroup, western Montana. Field trip guidebook T334:International Geological Congress 28th,Washington[C]. American Geophysical Union ,1989.46-69.
[24] Winston D. Evidences for intracratonic, fluvial and lacustrine setting of Middle to Late Proterozoic Laurentia-Baltica[J].Geological Association of Canada Special Paper,1990, 38:535-564.
[25] Schiber J. Facies and Deposition of a mixed terrigenous-carbonate suite in a Middle Proterozoic epicratonic sea: The Newland Formation. Belt Supergroup,Montana,USA[J]. Neues Jahrbuch Fur Geologie und Palaontologie Abhandlungen,1992,184:155-180.
[26] Smith A G,Barnes W C. Correlation of and facies changes in the carbonaceous, calcareous, and dolomitic formations of Precambrian Belt-Purcell Supergroup[J]. Geological Society of America Bulletin,1966,77: 1 399-1 426.
[27] Pratt B R.Shrinkage features (“molar tooth” structure) in Proterozoic limestones; new model for their origin through synsedimentary earthquake-induced dewatering[A]. In: Geological Society of America, 1992 Annual Meeting.Abstracts with Programs[C].Geological Society of America,1992,24(7):53. 
[28] Pratt B R,Winston D,Rittel J F,et al. Gas bubble and expansion crack origin of molar-tooth calcite structures in the middle Proterozoic Belt Supergroup, western Montana; discussion and reply[J].Journal of Sedimentary Research,1999,69(5)  :1 136-1 145.
[29] Pratt B R. Molar-tooth structure in Proterozoic carbonates rocks: Origin from synsedimentary earthquake and implications for the nature and evolution of basins and marine sedimentary[J].GSA Bulletin,1998,110(8):1 028-1 045.
[30] Rossetti D F,Goes A M. Deciphering the sedimentological imprint of paleoseismic events；an example from the Aptian Codo Formation,northern Brazil[A].In:Shiki T,Cita M B,Gorsline D S, eds. Seismoturbidites,Seismites and Tsunamiites[C]. Sedimentary Geology,2000,135(1~4):137-156.
[31] Daly R A. Geology of the North American Cordillera at the Forty-ninth Paralel[R].Canada Geological Survey Memoir 38,1912, partsⅠ-Ⅲ: 857.
[32] Eby D E. Carbonate sedimentation under elevated salinities and implications for the origin of “Molar-tooth” structure in the Middle Belt Carbonate Interval (Late Precambrian), northwestern Montana[J]. Abstracts with Programs Geological Society of America,  1975,7:1 063. 
[33] Horodyski R J. Stromatolites of the upper Siyeh Limestone (Middle Proterozoic), Belt Supergroup, Glacier National Park, Montana[J].  Precambrian Research, 1976, 3:517-536.
[34] Plummer P S,Gostin V A. Shrinkage cracks:Desiecation or synaeresis?  [J].Journal of Sedimentary Petrology,1981, 51:1 147-1 156.
[35] Hofmann H J. The mid-Proterozoic Little Dal macrobiota, Mackenzie Mountain,northwest Canada[J].  Paleontology, 1985, 28:280-300. 
[36] Failchild I J,Spiro B. Petrological and isotopic implications of some contrasting Late Precambrian carbonates NE Spitsbergen[J].Sedimentology, 1987, 34:973-989.
[37] Calver C R,Baillie P W. Early diagenetic concretion associated with the intrastratal shrinkage cracks in an upper Proterozoic dolomite, Tasmania, Australia[J]. Journal of Sedimentary Petrology, 1990,60:293-305.
[38] Cowan C A,James N P.Diastasis cracks: Mechanically Generated synaeresis-like cracks in Upper Cambrian shallow water oolite and ribbon carbonmates[J].Sedimentology,1992,39:1 101-1 118.
[39] Pratt B R. Proterozoic syneresis cracks and molar-tooth structure; formation by synsedimentary seismicity.Program with Abstracts - Geological Association of Canada[Ｒ].  Mineralogical Association of Canada; Canadian Geophysical Union, Joint Annual Meeting,1993.
[40] Gillson J L. Contact metamorphism of the rocks in the Pend Oreille district, northern Idaho[J].  US Geological Survey Professional Paper,1929,158-F:111-121.
[41] Ross C P. The geology of Glacier National Park and the Flathead region, northwestern Montana[J]. US Geological Survey Professional  Paper,1959,296:125.
[42] Pflug H D.Gesteinbildende organismen aus Molar Tooth Limestone der Beltserie (Praekambrium), Palaeontographica Abteilung B[J].Palaeophytologie,1968,121: 134-141.
[43] Horodyski R J. Paleontology of the Middle Proterozoic Belt Supergroup[A]. In: Winston D, Horodyski  R J, Whipple J W, eds. Middle Proterozoic Belt Supergroup, western Montana[C].Washington: American Geophysical Union,1989.7-26.
[44] Furniss G,Rittle J F,Winston D. Gas bubble and expansion crack origin of  “Molar-tooth” calcite structures in the Middle Proterozoic belt supergroup. western Montana[J].Journal of Sedimentary Research,1998,68(１):104-114.
[45] Frank T D.  Lyons-Timothy-W. “Molar-tooth” structures: A geochemical perspective on a Proterozoic enigma[J]. Geology (Boulder),1998,26(8):683-686.