The Pb-Pb Isochron Age of the Kuangshishan Formation in Shennongjia Area on the Northern Margin of the Yangtze Craton and Its Geological Implications
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摘要: 扬子克拉通北缘神农架地区出露了大量中元古代碳酸盐岩地层,但已有的同位素年代学资料有限,故对神农架群矿石山组白云岩开展了全岩Pb-Pb等时线测年.研究结果表明,矿石山组白云岩206Pb/204Pb变化范围相对较大,为18.753~23.106,而207Pb/204Pb和208Pb/204Pb则变化范围相对较小,分别为15.606~16.046和37.793~38.599.八件白云岩样品206Pb/204Pb和207Pb/204Pb之间呈良好的线性关系,构成Pb-Pb等时线年龄为1632±75Ma(MSWD=8.7),代表了矿石山组地层主体沉积时代,与已有的年代学结果可对应,表明Pb-Pb同位素体系可对古老的碳酸盐岩地层进行较为精确地定年.结合前人对于神农架群的年代学资料,确定神农架群的沉积时限应为1600~1100Ma的中元古代.Abstract: The Shennongjia Group, located on the northern margin of the Yangtze Craton, shows a series of well-preserved succession of the Mesoproterozoic carbonate strata. However, geochronological data collected from this area are limited. In this study, we report a Pb-Pb isochron age for the Kuangshishan Formation of the Shennongjia Group. The 206Pb/204Pb ratios of the dolostone of the Kuangshishan Formation show wide variations from 18.753 to 23.106. On the contrary, the 207Pb/204Pb ratios and the 208Pb/204Pb ratios have a limited range from 15.606 to 16.046 and 37.793 to 38.599, respectively. 8 dolostone samples data show an obvious linear relationship between 206Pb/204Pb and 207Pb/204Pb, yielding a Pb-Pb isochron age of 1632±75Ma (MSWD=8.7) which represent the depositional age for the Kuangshishan Formation. This age accords well with previous published data, indicating that a precise stratigraphic age of the ancient carbonate strata can be obtained through Pb-Pb dating technique. Combined with previous researches, we suggest that the age span of the Shennongjia Group is 1600 to 1100Ma of Mesoproterozoic.
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Key words:
- Shennongjia Group /
- Kuangshishan Formation /
- Pb-Pb isochron /
- Mesoproterozoic /
- carbonate /
- petrology
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图 2 神农架地区中元古代地层柱状图及采样点位
1.砾岩;2.砂砾岩;3.砂岩;4.粉砂岩;5.页岩/板岩;6.燧石;7.石灰岩;8.白云岩;9.角砾状白云岩;10.硅质条带白云岩;11.叠层石白云岩;12.火山岩;13.凝灰岩;14.整合接触关系;15.平行不整合接触关系;16.采样点;据李怀坤等(2013) 修改
Fig. 2. Mesoproterozoic stratigraphic histogram of the Shennongjia area and the sampling locations of the Kuangshishan Formation
表 1 神农架群矿石山组Pb同位素组成
Table 1. Pb isotope compositions of carbonate rocks from the Kuangshishan Formation, Shennongjia Group
序号 样号 岩性 206Pb/204Pb 2δ 207Pb/204Pb 2δ 208Pb/204Pb 2δ 1 12SNJ-72 块状白云岩 19.038 0.005 15.641 0.004 38.135 0.006 2 12SNJ-73 含黑色叠层石白云岩 19.774 0.005 15.707 0.004 37.897 0.008 3 12SNJ-75 块状白云岩 18.753 0.002 15.606 0.002 37.793 0.004 4 12SNJ-76 块状白云岩 20.322 0.007 15.740 0.006 38.341 0.009 5 12SNJ-77 含黑色叠层石白云岩 18.433 0.004 15.625 0.004 38.241 0.010 6 12SNJ-78 泥质条带白云岩 23.106 0.003 16.046 0.002 38.100 0.005 7 12SNJ-81 泥质条带白云岩 19.621 0.005 15.711 0.004 38.016 0.007 8 12SNJ-83 含叠层石白云岩 19.786 0.006 15.719 0.008 38.599 0.003 9 12SNJ-84 块状白云岩 21.076 0.005 15.830 0.004 38.114 0.001 -
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