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下面选编的几张照片是新疆北部不同地区、不同地质时代的枕状熔岩。 1和2表示西准噶尔唐巴勒地区中奥陶统科克沙依组中的枕状熔岩。在岩枕的表面往往有一层厚约0.5厘米的球颗玄武岩。岩枕与岩枕之间凝灰物质很少。 3表示西准噶尔萨尔托海下石炭统火山岩组中的枕状熔岩。出露于断层旁,被构造劈理强烈破坏。 4和5表示阿勒泰镇中泥盆统枕状熔岩,已变质成辉石角闪片岩;但枕状结构仍完好地保
Selected below a few photos of different parts of northern Xinjiang, different geological times pillow lava. 1 and 2 represent pillow lava in the Middle Ordovician Coxhayi Formation in the Tangbaler area, western Junggar. The surface of the rock pillow often has a layer of pellets about 0.5 cm thick basalt. There is very little tuff material between the rock pillows and the rock pillows. 3 indicates pillow-shaped lava in the Lower Carboniferous volcanic rocks in Salto, West Junggar. Exposed to the fault, was strongly damaged by cleavage. 4 and 5 indicate that the middle Devonian pillow lava in Altay town had been metamorphosed into pyroxene hornblende; however, the pillow structure was still intact