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南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

王尹 李祥辉 周勇 刘玲

王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
引用本文: 王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
Citation: WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012

南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

doi: 10.14027/j.cnki.cjxb.2015.01.012
基金项目: 国家自然科学基金项目(批准号:41372106)和国际重点基础研究发展计划“973”项目(编号:2012CB822003)联合资助
详细信息
    作者简介:

    王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

  • 中图分类号: P532

Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin

  • 摘要: 利用陆源沉积中的碎屑组份(泥岩中的碎屑黏土矿物种类和砂岩中砂、粉砂碎屑类型)相对含量变化,对广东北部和江西南部的南雄盆地晚白垩世—古新世古气候进行了分析.结果显示,砂岩碎屑组份含量气候指数(长石/石英比,F/Q)介于0.02~0.14之间;(碎屑)黏土矿物组合主要以伊利石为主,平均79%;伊利石结晶度指数与化学指数分别为0.25~0.39、0.31~0.7.进一步分析表明,研究区这一时期以干旱气候为主,存在暖湿气候间断,古气候演化可分为三个阶段:晚白垩世马斯特里赫特期以干旱—半干旱性气候为主,古新世丹尼期早期转变为相对湿热或与干旱—半干旱气候交替,古新世丹尼期晚期恢复到半干旱性气候,但比第一阶段湿度可能稍有增加.这一总体干旱—半干旱气候格局及其变化总体与同期全球气候变化一致.
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  • 收稿日期:  2013-12-09
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  • 刊出日期:  2015-02-10

目录

    南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示

    doi: 10.14027/j.cnki.cjxb.2015.01.012
      基金项目:  国家自然科学基金项目(批准号:41372106)和国际重点基础研究发展计划“973”项目(编号:2012CB822003)联合资助
      作者简介:

      王尹 男 1985年出生 硕士 古气候与古土壤 E-mail: yin31721@qq.com

    • 中图分类号: P532

    摘要: 利用陆源沉积中的碎屑组份(泥岩中的碎屑黏土矿物种类和砂岩中砂、粉砂碎屑类型)相对含量变化,对广东北部和江西南部的南雄盆地晚白垩世—古新世古气候进行了分析.结果显示,砂岩碎屑组份含量气候指数(长石/石英比,F/Q)介于0.02~0.14之间;(碎屑)黏土矿物组合主要以伊利石为主,平均79%;伊利石结晶度指数与化学指数分别为0.25~0.39、0.31~0.7.进一步分析表明,研究区这一时期以干旱气候为主,存在暖湿气候间断,古气候演化可分为三个阶段:晚白垩世马斯特里赫特期以干旱—半干旱性气候为主,古新世丹尼期早期转变为相对湿热或与干旱—半干旱气候交替,古新世丹尼期晚期恢复到半干旱性气候,但比第一阶段湿度可能稍有增加.这一总体干旱—半干旱气候格局及其变化总体与同期全球气候变化一致.

    English Abstract

    王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    引用本文: 王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示[J]. 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
    Citation: WANG Yin, LI XiangHui, ZHOU Yong, LIU Ling. Paleoclimate Indication of Terrigenous Clastic Rock's Component during the Late Cretaceous-Early Paleocene in the Nanxiong Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
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