末次冰消期热带湖光岩玛珥湖古季风变化记录
Changes in tropical Asia monsoon during the last deglaciation
湖光岩玛珥湖沉积物中的火山灰保存了其原始形貌、原生的沉积和成分特征,是进行岩芯沉积物对比和定年的理想材料之一。
The tephra could not comprise ash layer in the sediments ; however , they were dispersed in the same depth of the core , which is located in27 .