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ＫＡＮＧ Ａｎ, ＺＨＵ Ｘｉａｏｍｉｎ, ＨＡＮ Ｄｅｘｉｎ, ＷＡＮＧ Ｙａｎｂｉｎ, ＫＡＮＧ Ｑｉａｎｇ. 2003: Ｑｕａｔｅｒｎａｒｙ ｓｐｏｒｏｐｏｌｌｅｎ ａｓｓｅｍｂｌａｇｅｓ ａｎｄ ｐａｌｅｏｃｌｉｍａｔｉｃ ｆｌｕｃｔｕａｔｉｏｎ ｉｎ ｔｈｅ Ｑａｉｄａｍ ｂａｓｉｎ. Geological Bulletin of China, 22(1): 12-15.
Citation: ＫＡＮＧ Ａｎ, ＺＨＵ Ｘｉａｏｍｉｎ, ＨＡＮ Ｄｅｘｉｎ, ＷＡＮＧ Ｙａｎｂｉｎ, ＫＡＮＧ Ｑｉａｎｇ. 2003: Ｑｕａｔｅｒｎａｒｙ ｓｐｏｒｏｐｏｌｌｅｎ ａｓｓｅｍｂｌａｇｅｓ ａｎｄ ｐａｌｅｏｃｌｉｍａｔｉｃ ｆｌｕｃｔｕａｔｉｏｎ ｉｎ ｔｈｅ Ｑａｉｄａｍ ｂａｓｉｎ. Geological Bulletin of China, 22(1): 12-15.
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Ｑｕａｔｅｒｎａｒｙ ｓｐｏｒｏｐｏｌｌｅｎ ａｓｓｅｍｂｌａｇｅｓ ａｎｄ ｐａｌｅｏｃｌｉｍａｔｉｃ ｆｌｕｃｔｕａｔｉｏｎ ｉｎ ｔｈｅ Ｑａｉｄａｍ ｂａｓｉｎ

  • Ｃｈｉａｎ Ｎａｔｉｏｎａｌ Ｏｆｆｓｈｏｒｅ Ｏｉｌ Ｃｏｒｐｏｒａｔｉｏｎ， Ｂｅｉｊｉｎｇ 100021， Ｃｈｉｎａ;2. Ｇｅｏｓｃｉｅｎｃｅ Ｄｅｐａｒｔｍｅｎｔ， Ｕｎｉｖｅｒｓｉｔｙ ｏｆ Ｐｅｔｒｏｌｅｕｍ， Ｂｅｉｊｉｎｇ 102200， Ｃｈｉｎａ;3. Ｒｅｓｏｕｒｃｅ Ｄｅｖｅｌｏｐｍｅｎｔ Ｄｅｐａｒｔｍｅｎｔ， ＣＵＭＴ， Ｂｅｉｊｉｎｇ 100083， Ｃｈｉｎａ;4. Ｃｈｉｎａ Ｎａｔｉｏｎａｌ Ｏｉｌ ａｎｄ Ｇａｓ Ｅｘｐｌｏｒａｔｉｏｎ ａｎｄ Ｄｅｖｅｌｏｐｍｅｎｔ Ｃｏｒｐｏｒａｔｉｏｎ， Ｂｅｉｊｉｎｇ 100011， Ｃｈｉｎａ

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  • Ｔｈｅ Ｑｕａｔｅｒｎａｒｙ ｏｆ ｔｈｅ Ｑａｉｄａｍ ｂａｓｉｎ ｉｓ ａ ｓｕｃｃｅｓｓｉｖｅ ａｎｄ ｃｏｍｐｌｅｔｅ ａｃｃｕｍｕｌａｔｉｏｎ ｏｆ ｆｌｕｖｉａｌ－ｌａｃｕｓｔｒｉｎｅ ｓｅｄｉｍｅｎｔｓ ｗｉｔｈ ａ ｇｒｅａｔ ｔｈｉｃｋｎｅｓｓ． Ｂａｓｅｄ ｏｎ ａ ｓｔｕｄｙ ｏｆ Ｑｕａｔｅｒｎａｒｙ ｓｐｏｒｏｐｏｌｌｅｎ ａｓｓｅｍｂｌａｇｅｓ ａｎｄ ｔｈｅｉｒ ｖｅｒｔｉｃａｌ ｄｉｓｔｒｉｂｕｔｉｏｎ ａｔ ｔｙｐｉｃａｌ ｐｒｏｆｉｌｅｓ ｏｆ ｈｏｌｅｓ ＺＫ７０１＋８０１， Ｓｈｕｉ ６， Ｓｅｚｈｏｎｇ ６ ａｎｄ Ｓｅｓｈｅｎ １， ｔｈｉｓ ｐａｐｅｒ ｄｉｓｃｕｓｓｅｓ ｉｎ ｄｅｔａｉｌ Ｑｕａｔｅｒｎａｒｙ ａｓｓｅｍｂｌａｇｅ ｚｏｎｅｓ ａｎｄ ｔｈｅ ｖｅｇｅｔａｔｉｏｎ ａｎｄ ｃｌｉｍａｔｉｃ ｅｖｏｌｕｔｉｏｎ ｒｅｐｒｅｓｅｎｔｅｄ ｂｙ ｔｈｅｍ． Ａ ｈｉｇｈｌｙ ｐｒｅｃｉｓｅ ｓｐｏｒｏｐｏｌｌｅｎ ｃｌｉｍａｔｅ ｃｕｒｖｅ ｉｓ ｏｂｔａｉｎｅｄ， ｗｈｉｃｈ ｓｈｏｗｓ ｔｈａｔ ａｌｔｅｒｎａｔｉｏｎ ｏｆ ｄｒｙ－ｃｏｌｄ ａｎｄ ｗｅｔ－ｗａｒｍ ｃｌｉｍａｔｅｓ ｉｓ ｔｈｅ ｂａｓｉｃ ｍｏｄｅｌ ｏｆ ｔｈｅ Ｑｕａｔｅｒｎａｒｙ ｐａｌｅｏｃｌｉｍａｔｅ ｅｖｏｌｕｔｉｏｎ ｉｎ ｔｈｅ Ｑａｉｄａｍ ｂａｓｉｎ． Ａｌｔｏｇｅｔｈｅｒ ５９ ｓｐｏｒｏｐｏｌｌｅｎ ａｓｓｅｍｂｌａｇｅ ｚｏｎｅｓ ａｎｄ ２９ ｃｏｍｐｌｅｔｅ ｃｏｌｄ－ｗａｒｍ ｐａｌｅｏｃｌｉｍａｔｉｃ ｃｙｃｌｅｓ ｓｉｎｃｅ １．８７ Ｍａ Ｂ．Ｐ． ｈａｖｅ ｂｅｅｎ ｒｅｃｏｇｎｉｚｅｄ． Ｔｈｅｙ ｃａｎ ｂｅ ｗｅｌｌ ｃｏｒｒｅｌａｔｅｄ ｗｉｔｈ ｔｈｅ ３７ ｐａｌｅｏｃｌｉｍａｔｅ ｃｙｃｌｅｓ ｄｅｒｉｖｅｄ ｆｒｏｍ Ｑｕａｔｅｒｎａｒｙ ｌｏｅｓｓ ａｎｄ ｐａｌｅｏｓｏｌｓ ｉｎ ｎｏｒｔｈｗｅｓｔｅｒｎ Ｃｈｉｎａ ａｎｄ ｔｈｅ ｄｅｅｐ ｓｅａ ｏｘｙｇｅｎ ｉｓｏｔｏｐｅ ｃｌｉｍａｔｅ ｒｅｃｏｒｄｓ．
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