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在褶皱完成区和活动地台上发育的负向构造在许多情况下也能控制岩浆活动。这类构造分为继承坳陷和上迭盆地。继承坳陷——这是年轻地台盖层范围内的负向构造,它继承着基底构造,也就是说,是在复向斜上发育的(1964)。但是岩浆过程多半发生在上迭盆地里。上迭盆地切过基底构造,而如果和基底构造有共同的方位,那也不是与和它同一符号
The negative tectonics developed in the zone of fold completion and the active platform can in many cases also control magmatic activity. These structures are divided into inherited depressions and the Upper Dietian Basin. Inherited Depressions - This is a negative tectonic setting within the young platform cover that inherits the basement structure, that is, develops on the syncline (1964). However, most of the magmatic processes occurred in the Upper Dietian basin. The Basalt basin cuts through the basement structure, and if it has a common orientation with the basement structure, it is not the same sign as it