rapakivi

rapakivi

美 　英

• 网络奥环斑花岗岩；奥长环斑花岗岩；更长环斑花岗岩

例句

This suggests that the typical rapakivi texture can be formed in various epochs and different tectonic settings.

亦表明典型的环斑结构可以出现于不同的时代和构造环境。

Recent studies show, however, that rapakivi granites can be formed in age from Archaean to Phanerozoic and can even occur in orogen.

环斑花岗岩既可以出现于从太古代到显生宙的各个地质时期，也可以产生于造山带中。

A Study of Biotite from the Shahewan Rapakivi Granite in Qinling and Its Significance

秦岭沙河湾环斑花岗岩中黑云母的研究及其意义

Zircon U-Pb ages and Hf isotopes and their geological significance of the Miyun rapakivi granites from Beijing, China

北京密云环斑花岗岩锆石U-Pb年龄和Hf同位素及其地质意义

Characteristics of Rapakivi Texture in Mesozoic Shahewan Granite of North Qinling Mountains and Some Related Problems

北秦岭中生代沙河湾岩体环斑结构特征及有关问题的讨论

A Query about So-called Rapakivi Granites in the Qinling Orogen

对秦岭奥长环斑花岗岩的质疑