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Zhou Bengang (Insitute of Geology,China Seismological Bureau,Beijing 100029)Liu Tanzhuo (Lamont Doherty Earth Observatory of Columbia university,Palisades,NY10964, USA)Zhang Yuming (Insitute of Geology, China Seismological Bureau,Beijing 100029)  
We collected 100 rock varnish samples from the northern Tian Shan for ultra-thin sectioning. Laterally continuous dark and orange microlaminations are observed in these ultra-thin sections of rock varnish. Microprobe chemical analyses indicate that dark layers in the varnish are rich in Mn and orange layers are poor in Mn. Microscopic examinations of varnish ultra-thin sections reveal a lamination pattern that is regionally consistent and comparable. Based on paleoclimatic and geomorphic age control,the Late Pleistocene varnish lamination sequence is tentatively established and its chronological impications are explored as well.
【Fund】: 地震联合基金!(95233)
【CateGory Index】: P531
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