...Minerals in the YSDP102 Core on the Continental Sh..._维普网

来自 : www.cqvip.com/QK/87473A/200400 发布时间：2021-03-25

摘 要：Ninety-eight clay mineral samples from the YSDP102 core were analyzed by x-ray diffractometer to study the four clay minerals: illite, chlorite, kaolinite and smectite. Twenty-eight samples had been analyzed on the laser particle-size analyzer to reveal the particle features of the sediments. Distribution of the clay minerals and the particle characteristics in the YSDP102 core show that the core experienced three different depositional periods and formed three different sedimentary intervals due to different sediment sources and different depositional environments. Features of the clay minerals and the heavy minerals in the YSDP102 core indicate that coarse-grained sediments and fine-grained sediments result from different sources. The Yellow Sea Warm Current has greatly influenced the sedimentary framework of this region since the current\'s formation.
Ninety-eight clay mineral samples from the YSDP102 core were analyzed by x-ray diffractometer to study the four clay minerals: illite, chlorite, kaolinite...JIANGXuejun QUGaosheng LIShaoquan 黏土矿石 黄海暖流 沉积环境 水团 高岭波动 Features of Clay Minerals in the YSDP102 Core on the Continental Shelf of the Southeast Yellow SeaNinety-eight clay mineral samples from the YSDP102 core were analyzed by x-ray diffractometer to study the four clay minerals: illite, chlorite, kaolinite and smectite. Twenty-eight samples had been an...Features of Clay Minerals in the YSDP102 Core on the Continental Shelf of the Southeast Yellow Sea