Typical slump structure was found in orebody No, 11 at the juncture of the two deposits.
在两个矿床接合部位的11号矿体中,发现一套典型的小型滑塌构造,其变形层为薄层菱铁矿,非变形层为条带状重晶石岩,两者均为海底喷流成因的热水沉积而成。
It consists of clustered comagmatic source volcanic apparatuses of fissutr type,volcanic collapse structure and glug of passive emplacement,There are five eruptive depositional and oruptive filling stages,The primary roc.
它包括同源成串的裂隙式火山机构、火山塌陷构造和塌陷被动侵位的岩塞。
