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地质学报  2008 

燕山构造带凤山盆地早白垩世的沉积过程

, PP. 769-777

Keywords: 燕山构造带,早白垩世,凤山盆地,沉积过程

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Abstract:

凤山盆地是燕山构造带内的一个早白垩世伸展盆地。盆地内沉积岩相和相组合的详细分析结果显示,盆地内部发育不同的沉积相带,并显示明显的空间变化。盆地北部和西部边缘以冲积扇砾岩和扇三角洲砂岩、砾岩沉积为主,盆地中心为湖泊细粒沉积。古流向和物源恢复结果证明,盆地沉积物主体来自北部和西部变质岩基底。盆地构造沉降和沉积过程主要受北缘和西缘张性断层的控制。断层下盘基底岩石的抬升与盆地边界正断层活动相关,从而成为盆地主要的物源区。凤山盆地的演化可划分为3个阶段,即早期火山喷发阶段、中期强烈断陷阶段和晚期填平阶段。

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