首页> 外文OA文献 >Clay Mineralogy of Red Clay Deposits from the Central Carpathian Basin (Hungary): Implications for Plio/Pleistocene Chemical Weathering and Paleoclimate
【2h】

Clay Mineralogy of Red Clay Deposits from the Central Carpathian Basin (Hungary): Implications for Plio/Pleistocene Chemical Weathering and Paleoclimate

机译:来自喀尔巴阡中部盆地(匈牙利)的红粘土矿床的粘土矿物学:对上新世/更新世化学风化和古气候的影响

摘要

Geochemical and mineralogical studies of palaeosols provide essential information for palaeoclimatic and palaeoenvironmental interpretation of continental deposits and can present a proxy for palaeoclimate. Red clays in the central Carpathian Basin (Hungary) (Tengelic Red Clay Formation; Kerecsend Red Clay Formation), overlain by loess-palaeosol sequences, were studied. Results from geochemical climofunctions applied to Upper Pliocene–Lower Pleistocene red clays and palaeosols located in the Carpathian Basin, and clay mineralogy, indicate that the palaeoclimate was considerably more humid and warmer during the Late Pliocene-Early Pleistocene in comparison to modern values.
机译:古土壤的地球化学和矿物学研究为大陆性沉积物的古气候和古环境解释提供了必要的信息,并可以为古气候提供一个代表。研究了喀尔巴阡盆地中部(匈牙利)的红粘土(Tengelic红粘土组; Kerecsend红粘土组),其上覆有黄土-古土壤层序。地球化学气候函数的结果应用于喀尔巴阡盆地的上新世-下更新世红粘土和古土壤以及粘土矿物学,表明与现代值相比,上新世晚期-早更新世的古气候明显更湿和更温暖。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号