深水等深流沉积中记录的米兰科维奇特性——以陕西富平地区上奥陶统赵老峪组为例
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摘要
陕西富平地区上奥陶统赵老峪组为深水盆地边缘至深水斜坡沉积环境,发育深水原地沉积、等深流沉积及重力流沉积。以野外实测剖面、岩相特征等资料为基础,结合米兰科维奇理论、天文地层学、古海洋学以及古气候学,系统研究该地区等深流强度与古气候、海平面、古盐度的关系。结果表明:Fischer图解可以客观、准确地反映深水沉积地层相对海平面变化;深水沉积及等深流沉积中不同级次旋回垂向组合关系记录了米兰科维奇特性,即小级别旋回在垂向上有序地按照1∶4或者1∶5的形式叠加构成较大级别旋回;等深流强度受米兰科维奇旋回影响,呈多周期弱→强→弱递变;等深流强化周期约为0.1Ma。
The Upper Ordovician Zhaolaoyu Formation in Fuping area of Shaanxi develops the deep water autochthonous deposits,contourites and gravity-flow deposits,and the sedimentary environment is from the edge of the deep water basin to deep water slope.On the basis of the section measured in field and the lithofacies features,combined with Milankovitch theory,astrostratigraphy,paleoceanography,paleoclimatology and Fischer diagram,the relationships between the intensity of the contour current and changes of paleoclimate,sea level and paleosalinity were studied.The results show that Fischer diagram can reflect sea level changes objectively and accurately;the vertical combination of different grades of cycle in the deep water sediments and contourites records the characteristics of Milankovitch,showing that small scale cycles are superimposed in the vertical direction in the form of 1∶4 or 1∶5 to form the largerlevel of cycles;the contour current intensity is affected by Milankovitch cycle,which is reflected in the multi-cycle of weak-strong-weak change;the activity cycle of contour current is about 0.1Ma.
The Upper Ordovician Zhaolaoyu Formation in Fuping area of Shaanxi develops the deep water autochthonous deposits,contourites and gravity-flow deposits,and the sedimentary environment is from the edge of the deep water basin to deep water slope.On the basis of the section measured in field and the lithofacies features,combined with Milankovitch theory,astrostratigraphy,paleoceanography,paleoclimatology and Fischer diagram,the relationships between the intensity of the contour current and changes of paleoclimate,sea level and paleosalinity were studied.The results show that Fischer diagram can reflect sea level changes objectively and accurately;the vertical combination of different grades of cycle in the deep water sediments and contourites records the characteristics of Milankovitch,showing that small scale cycles are superimposed in the vertical direction in the form of 1∶4 or 1∶5 to form the largerlevel of cycles;the contour current intensity is affected by Milankovitch cycle,which is reflected in the multi-cycle of weak-strong-weak change;the activity cycle of contour current is about 0.1Ma.
引文
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