沉积岩中的缝合线构造有原生和次生两种成因。
There are primary stylolite and secondary stylolite in sedimentary rocks.
滇西地区的构造格局具有一定的规律性，造山带与缝合线相间分布。
The tectonic situation in Western Yunnan is of certain regulation with the interlacing distribution of orogenic zone and seam.
给定两个欲合并的网格，先由它们的边界三角形构造一条缝合线，再以该缝合线为骨架构造连接这两个网格的缝合面。
Given a two meshes which want to be merged, we firstly construct a stitch line derived from their fringe triangles, and then create stitch faces which adhere to this stitch line to connect them.
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