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- W1567458449 abstract "Caocun () Zhangbianyuan 的黄土侧面() 在黄土高原的东南边缘被定位，它是在 Sanmenxia 的黄土阶层的一个典型代表() 区域。在 145 m 厚侧面，一个 loess-paleosol 序列从 L1 发生到 L33，在下面由一张红色粘土床躺着。B/M 边界在红色粘土附近在 L33 的底部在 L7，在到 S12 的 S11 的 Jaramillo 事件，在到 L26 的 L23 的 Olduval 事件，和 M/G 边界的底部被记录。黄土存款的磁化率，以及碳酸盐和颗粒度部件，显示有许多周期的古气候变化，包括 13 个冷事件的一个总数，那各持续了超过 40 000 一。高分辨率的 chronostratigraphic 侧面根据谷物特征用一个年龄模型被建立了。清楚的关联从 3X10 (5 ) 在 Caocun 黄土继任和 SPECMAP 在 paleomonsoon 的记录之间存在 B. P。到礼品。Caocun 侧面能在东南的黄土高原充当一个控制地点。它的 paleoenvironmental 记录联系到东方亚洲 paleomonsoon 理论。给词调音：Sanmenxia 黄土；磁电机地层学；paleomonsoon 记录；paleoenvironmental 变化" @default.
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- W1567458449 date "2006-01-01" @default.
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- W1567458449 title "Sanmenxia Loess and Paleoenvironmental Change" @default.
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