辉绿玢岩是冈瓦纳被动陆缘在晚古生代裂解的产物。
Diabase-porphyrite was the splitting product of passive margin of Gondwana Continent in Late Jurassic.
黑龙江省鸡西盆地张新地区辉绿玢岩呈岩床状侵入晚中生代城子河组地层中；
The Chengzihe Formation in Zhangxin area of Jixi basin, Heilongjiang Province is intruded by the algorite sill.
黑龙江省鸡西盆地张新地区辉绿玢岩呈岩床状侵入晚中生代城子河组地层中；
The Chengzihe Formation in Zhangxin area of Jixi basin, Heilongjiang Province is intruded by the algorite sill.
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