| 吕梁－陕北地区马家沟组中小层序特征及其成因 |
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| 引用本文： | 高永丰,魏瑞华.吕梁－陕北地区马家沟组中小层序特征及其成因[J].沉积学报,1995,13(3):32-38. |
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| 作者姓名： | 高永丰 魏瑞华 |
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| 作者单位： | 河北地质学院 石家庄 050031 |
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| 摘 要： | 吕梁－陕北地区马家沟组碳酸盐岩－蒸发岩向上变浅层序由一系列小层序垂向叠置而成。本文主要通过小层序特征及其分布规律的研究，认为小层序是由叠加在三级海平面变化旋回上的频繁小级别海平面升降旋圆形成的，这种小级别海平面旋回与地球轨道旋回引起的米兰科维奇旋回有关。
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| 关 键 词： | 小层序 海平面变化旋回 碳酸盐岩 马家沟组 |
| 收稿时间： | 1994-11-01 |
The Characteristics and Origin of Small-scale Sequences in Majiagou Formation(Middle Ordovician)in the L liang-Norhern Shaanxi Area |
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| Institution: | Hebei College of Geology, Shijiazhuang 050031 |
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| Abstract: | Shallowing-upward sequences in the Majiagou carbonates in the Luuliang-Northen Shaanxi area consist of a great number of small-scale sequences. The small-scale sequences (1.2-5min thickness) are the fundamental units of the Majiagou sedimentary deposit. The small-scale sequences have obvious boundaries of abrupt change tO deeper facies, and are of internally regressive deposits,containing little or no transgressive deposits. The small-scale sequences are vertically stucked and laterally extensive asymmetry cycles for tens of kilometers (independent of lateral facies). These sequences appear to occur in the depositional facies of most environments.Six types of small-scale sequences Can be recognized, i. e., A: trace-fossil cycles in deeper open sea subtidal facies; B:dilution cycles of hypersaline brine in deeper lagoon factes; C:intertidel to supratidal overprinting of shallow subtidal factes:D: intertidal to supratldal ovetprining of shallow brackish subtidal factes, ofen associated with early dolomitization; E: Sabkha sequences; F:terrestrial overprinting of intertidal factes. The characteristics and distribution of small- scale sequences were formed during high-frequency but low-amplitude sea level variations superimposedon the third order transgressive - cycles. The types of the small-scale sequences depend on the position of high- frequency sea level variations within the third order cycles and the palaeotopography of sedimentary environments. During the high sea level of long-term cycles periodically changed the physical-chemical conditions of water body in deeper open sea subtidal racies. Thus small-scale sequences recorded the benthic and in fauna response to trasgressiveregressive cycles. In shallow peritidal environments during the longer-term sea level fall, highfrequency sea level variations made the ralative sea level reach the critical water depth. Consequently, C. D. E. F small-scale sequences were formed. In local depressions, the highfrequency sea level rise provided the punctuated supplement of sea water for the evaporation and caused the dilution cycles of hypersaline brine which formed B small- scale sequences. Highfrequency small-scale sea level variations seem to be related to Milankovitch climatic cycles caused by the Earth's orbital cycles. identification and correlation of sequence boundaries make it possible to set up a framework of isochronous surfaces, and thus to interpret in derail the palaeographic,sedimentological evolution of the Majiagou carbonate environments and to predict the distribution of oil-gas reservoirs in the sedimentary basin. |
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