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作 者:金秉福[1] 林振宏[1] 时振波[1] 林晓彤[1]
机构地区:[1]中国海洋大学海洋地球科学学院
出 处:《古地理学报》2004年第3期372-379,共8页Journal of Palaeogeography:Chinese Edition
基 金:国家自然科学基金项目 (批准号 :40 0 760 13 )资助
摘 要:对东海外陆架中部表层沉积物 34个样品 ,南部两个岩心 75个样品的沉积物特征和重矿物特征进行了分析 ,计算了其中有用重矿物砂的品位。东海外陆架晚更新世残留沉积中有用的重矿物砂来源于中国大陆 ,其含量与细砂含量、重矿物总量、沉积物的粒度和分选性呈正相关关系。重矿物砂赋存在海退层位中 ,形成于滨岸带 ,并经过后期海侵过程的改造和进一步富集 ,主要分布在水深 10 0~ 2 0 0m范围内。外陆架中部有用重矿物砂高品位异常区面积达 1 2× 10 4km2 ,锆石和石榴石品位达到Ⅰ级异常。南部岩心中异常品位的有用重矿物砂的厚度 1 5~ 2m ,锆石品位达到工业边界品位 ,研究区钛铁矿普遍出现Ⅱ级和Ⅱ级以上的异常品位。东海外陆架区浅海砂矿成矿条件较好 ,具有较大的资源潜力 。Thirty-four samples were collected from surface sediments on outer shelf of the middle East China Sea,and 75 samples were collected from two cores of outer shelf of the southern East China Sea The characteristics of sediments and heavy minerals of these samples have been studied,and grades of valuable heavy minerals in these samples are calculated The results show that valuable heavy minerals in relict sediments from the outer shelf of the East China Sea during the Late Pleistocene were derived from the continent of China The content of valuable heavy minerals is closely related to the content of fine sand and the total heavy minerals,grain size and sorting of the sediments Heavy minerals occured in regressive sequence in the littoral zone,and had been reworked and enriched by late transgressive process They are mostly distributed between 100 m and 200 m of water depth The high grade valuable heavy minerals cover an area of about 1 2×10 4 km 2 The grades of zircon and garnet have reached the order Ⅰanomaly of marine placer,and the thickness of valuable heavy minerals bearing sand in southern cores range from 1 5 to 2 meters Zircon has met boundary grade(≥0 5 kg/m 3 ),and the grade of ilmenite is commonly up to order Ⅱ and above order Ⅱ anomaly in the study area The conditions to form marine placer on the outer shelf are favorable The placer resource is considered to have a good economic potential and it is worth further investigation on the outer shelf of the East China Sea,especially along southern outer shelf
分 类 号:P534.631[天文地球—第四纪地质学] P736.21[天文地球—古生物学与地层学]
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