Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.
古
磁测量表明,中国新近系保德
界线层型,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。
质】新第三纪的(迄今2200至250万年前间,许

哺乳动物和早先形态的人类在这一时期出
);新近纪的(等于Neocene)Paleomagnetic measurements demonstrate that the Jijiagou section which is the stratotype one of Baode Stage of the Neogene in China records 12 normal and 11 reversed polarity zones.
古
磁测量表明,中国新近系保德
界线层型,山西保德冀家沟剖面记录了12个正极性段与11个负极性段。
The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.
“盆
”构造发育模式为:从晚侏罗世到白垩纪末期发育的山间“盆
”
、发展到早第三纪断陷湖盆的发育、再演化为晚第三纪及第四纪
陷发育
段。
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