摘要
滦平盆地可与中国东部含能源盆地类比 ,其在构造发育上经历了 5个阶段 ,各阶段具有不同的盆地充填特点。盆地发育的动力学分析表明 ,中国东部中生代盆地发育的动力学因素包括深部高热流和厚地壳 ,以及板块间相互作用变化而导致的构造应力场的改变。滦平盆地构造活动通过改变湖水深度。
The Luanping basin shows some analogy to the energy bearing basins in eastern China. It underwent 5 stages in the tectonic development during its formation.Each stage has different characteristic on the aspect of basin filling.The analysis of basin development shows that the dynamic background influencing the development of Mesozoic basins in eastern China includes high heat flow in the deep,thick earth crust,as well as changes of the tectonic stress field due to interaction between the plates.The changes of lacustrine water depth and palaeoslope induced by the tectonic activities combining with the palaeoclimate control the evolution of the fan deltic deposition systems in the Luanping basin.
出处
《现代地质》
CAS
CSCD
北大核心
2000年第2期179-184,共6页
Geoscience
基金
国家"九五"重点科技攻关项目之专题研究"扇三角洲沉积体系三维研究及储层特征"! (编号 :95- 10 9- 0 1-0 1)
