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热液石英脉呈塊状結构为大家所熟知。国內已有文献中皆認为它属于原生成因,且为高温石英脉的特征。苏联維尔圖什科夫曾于1946年研究烏拉尔無矿石英脉时提出塊状結构系次生的,并指出原生结构具有柱状特征。但他的这种看法:“塊状結构系后期构造破坏所引起的变化及变質作用的結果”在苏联尚有爭論。我国赣南石英脉的塊状結构被视为原生成因,但并未经詳細研究。作者在該区进行了初步观察及整理,特提出下列簡短报导。
Quartz veins have a massive structure known to all. In the domestic literature, it is considered that it belongs to the original genesis, and is characterized by high temperature quartz veins. In the 1946 study of the Ural ore-free quartz vein, the Soviet Union Wertushkov proposed the secondary structure of the massive structure and pointed out that the primary structure has a columnar characteristic. However, his view is that “there is still controversy in the Soviet Union about the results of the changes caused by the post-tectonic destruction of massive structural systems and the metamorphism.” The massive structure of the quartz veins in southern Jiangxi Province is considered as a primordial cause, but it has not been studied in detail. The author conducted a preliminary observation and arrangement in the area, especially making the following brief reports.