The Baise basin is a typical pull-apart basin that was formed in Tertiary Period.
百色盆地是一典型的第三纪走滑拉分盆地。
Positive flower structure has been found in the Baise basin, and negative flower structure in the Jiuxi basin.
百色盆地的勘探实践已经发现了正花状构造的存在，在西西盆地还发现一个负花状构造。
The studies of the depositional characteristics showed that there are two different sedimentary systems in Baigang Formation in the eastern depression of Baise basin.
从露头分析和岩心观察入手，应用现代沉积学原理，对鄂尔多斯盆地东缘山西组二段露头和盆内岩心中的沉积序列及构造特征进行详细描述。
The studies of the depositional characteristics showed that there are two different sedimentary systems in Baigang Formation in the eastern depression of Baise basin.
从露头分析和岩心观察入手，应用现代沉积学原理，对鄂尔多斯盆地东缘山西组二段露头和盆内岩心中的沉积序列及构造特征进行详细描述。
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