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DATES AND RATES IN ANCIENT LAKES - AR-40-AR-39 EVIDENCE FOR AN EARLY CRETACEOUS AGE FOR THE JEHOL GROUP, NORTHEAST CHINA
SMITH, PE; EVENSEN, NM; YORK, D; CHANG, MM; JIN, F; LI, JL; CUMBAA, S; RUSSELL, D; SMITH, PE (reprint author), UNIV TORONTO,DEPT PHYS,60 ST GEORGE ST,TORONTO,ON M5S 1A7,CANADA.
1995-09-01
发表期刊CANADIAN JOURNAL OF EARTH SCIENCES
ISSN0008-4077
卷号32期号:9页码:1426-1431
文章类型Article
摘要The correlation of freshwater sediments in small, fault-bound basins in Liaoning Province, northeast China, known as the Jehol (or Rehe) Group, has been a subject of debate for many years, with biochronological estimates ranging from Late Jurassic to the Cretaceous periods. We have applied the laser Ar-40-Ar-39 technique to volcanic intercalations and lacustrine sediments from the Yixian Formation at the base of the Jehol Group. Minerals and whole-rock chips from the upper parts of the Yixian Formation give concordant ages with a mean of 121.1 +/- 0.2 Ma (1 sigma). Ages for samples near the base of the Yixian Formation give 121.4 +/- 0.6 and 122.9 +/- 0.3 Ma, and appear to be synchronous or only slightly older than the top of the formation. Integrated ages of 122 Ma for glaucony from the lacustrine sediments lying stratigraphically between the upper and lower parts of the Yixian are in very good agreement with the absolute age framework provided by the volcanic units. Such disseminated facies of this clay show promise for directly dating lacustrine sediments. All of the above Ar-40-Ar-39 dates provide an absolute calibration of the Yixian Formation, and show that the whole formation was deposited entirely within Early Cretaceous time over an interval of no more than 2-3 Ma.; The correlation of freshwater sediments in small, fault-bound basins in Liaoning Province, northeast China, known as the Jehol (or Rehe) Group, has been a subject of debate for many years, with biochronological estimates ranging from Late Jurassic to the Cretaceous periods. We have applied the laser Ar-40-Ar-39 technique to volcanic intercalations and lacustrine sediments from the Yixian Formation at the base of the Jehol Group. Minerals and whole-rock chips from the upper parts of the Yixian Formation give concordant ages with a mean of 121.1 +/- 0.2 Ma (1 sigma). Ages for samples near the base of the Yixian Formation give 121.4 +/- 0.6 and 122.9 +/- 0.3 Ma, and appear to be synchronous or only slightly older than the top of the formation. Integrated ages of 122 Ma for glaucony from the lacustrine sediments lying stratigraphically between the upper and lower parts of the Yixian are in very good agreement with the absolute age framework provided by the volcanic units. Such disseminated facies of this clay show promise for directly dating lacustrine sediments. All of the above Ar-40-Ar-39 dates provide an absolute calibration of the Yixian Formation, and show that the whole formation was deposited entirely within Early Cretaceous time over an interval of no more than 2-3 Ma.
WOS标题词Science & Technology ; Physical Sciences
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关键词[WOS]SINGLE GRAINS ; BIOTITE ; RECOIL
收录类别SCI
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:A1995TF84800012
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/4081
专题中科院古脊椎所(2000年以后)
通讯作者SMITH, PE (reprint author), UNIV TORONTO,DEPT PHYS,60 ST GEORGE ST,TORONTO,ON M5S 1A7,CANADA.
作者单位1.INST VERTEBRATE PALEONTOL & PALEOANTHROPOL, BEIJING 100044, PEOPLES R CHINA
2.CANADIAN MUSEUM NAT, OTTAWA, ON K1P 6P4, CANADA
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SMITH, PE,EVENSEN, NM,YORK, D,et al. DATES AND RATES IN ANCIENT LAKES - AR-40-AR-39 EVIDENCE FOR AN EARLY CRETACEOUS AGE FOR THE JEHOL GROUP, NORTHEAST CHINA[J]. CANADIAN JOURNAL OF EARTH SCIENCES,1995,32(9):1426-1431.
APA SMITH, PE.,EVENSEN, NM.,YORK, D.,CHANG, MM.,JIN, F.,...&SMITH, PE .(1995).DATES AND RATES IN ANCIENT LAKES - AR-40-AR-39 EVIDENCE FOR AN EARLY CRETACEOUS AGE FOR THE JEHOL GROUP, NORTHEAST CHINA.CANADIAN JOURNAL OF EARTH SCIENCES,32(9),1426-1431.
MLA SMITH, PE,et al."DATES AND RATES IN ANCIENT LAKES - AR-40-AR-39 EVIDENCE FOR AN EARLY CRETACEOUS AGE FOR THE JEHOL GROUP, NORTHEAST CHINA".CANADIAN JOURNAL OF EARTH SCIENCES 32.9(1995):1426-1431.
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