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《JOURNAL OF STRATIGRAPHY》 1994-01
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On magnetostratigraphy of the borehole HR_(88-1) in Huairou area, Beijing

Li Longyin and Chen Huahui  
In order to give a systematic layering and determination of geological time to the borehole sequence, a sampling was made for palaeomagnetic dating with an average interval of 1.2-1.3m. By thermal demagnetization, 1137 geomagnetic element data were extracted from 400 original samples, comprehensive analyses on the data have resulted in a polarity column shown in Figure 4.As can be seen, the polarity column is evidently divisible into three members.The interval from the surface down to 142m depth represents the Brunhes normal polarity chron, which involves two reversed polarity subchrons corresponding to the depth of 16-18m and 33-36m. A C14 age of 19 580a obtained from the sample at the depth of 8.35m and two thermoluminescent datings of 69 500a and 102 000a respectively from the samples of 27m and 32m deep demonstrate that the above mentioned two reversed subchrons are equivalent to the Laschamp subchron and Black subThe range from 142 to 358.5m deep corresponds to the Matuyama reversed polarity chron, this chron was interrupted by two normal subchrons: the Jaramillo (172-185m) and Olduvai (279-304m), as evidenced by a comparative analysis.The Gauss normal polarity chron is shown from 358.5 to 505.27m deep in theborehole. It embraces a reversed subchron, the Kaena, limited within the interval of454-475m deep.The lithologic section of the borehole HR, includes the entire Pleistocene series and part of Pliocene series. According to the correlation of the polarity columnand the lithologic section, we believe that the sediments below 370m depth belongto the Upper Pliocene series which cover a time span of 2.48--3.0Ma. The LowerPleistocene Series ranges from the depth of 145--370m. which was formed during0.73--2.48Ma. The Middle and Upper Pleistocene Series correspond to the Brunhesnormal polarity chron. The time boundary between Middle and Upper Pleistocene Series is about 0.15Ma. Our definition for the N/Q boundary is approximately conformable with M/G boundary.
【CateGory Index】: P534
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