摘要
作者以中更新统实测剖面为例，分析了赣北彭山一带中更新统红土中的白色“蠕虫”状结构特征及其成因，认为其由“微裂隙水流淋溶”和（或）“植物微根系吸收”所形成。
Taking the measured section of middle Pleistocene series as an exam-ple, the authors analyze the features and its genesis of the white “vermi-form” textures in the middle Pleistocene series laterite,Pengshan,NorthJiangxi,and hold that it was formed as a result of“microfissure streamsieaching”and(or)“microrooting absorption”
出处
《江西地质》
1994年第2期130-134,共5页
Jiangxi Geology
