新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2014年
4期
522-524
,共3页
层序地层%可容纳空间%泥炭堆积%基准面%地下水位
層序地層%可容納空間%泥炭堆積%基準麵%地下水位
층서지층%가용납공간%니탄퇴적%기준면%지하수위
Sequence stratigraphy%Accommodation%Peat accomulation%Base level%Groundwater table
据国内外近海含煤岩系层序地层学研究成果，运用基准面正弦式变化和衡定泥炭堆积速率，图解不同可容纳空间条件下泥炭堆积特征，认为可容纳空间与泥炭堆积相互作用决定泥炭堆积和终止时间点、泥炭堆积持续时段及有利时期，理论上，任何体系域都有形成区域广泛分布煤层的可能。气候条件是衡量泥炭生长速率的指标，地下水位决定了泥炭堆积的潜在有效可容纳空间。
據國內外近海含煤巖繫層序地層學研究成果，運用基準麵正絃式變化和衡定泥炭堆積速率，圖解不同可容納空間條件下泥炭堆積特徵，認為可容納空間與泥炭堆積相互作用決定泥炭堆積和終止時間點、泥炭堆積持續時段及有利時期，理論上，任何體繫域都有形成區域廣汎分佈煤層的可能。氣候條件是衡量泥炭生長速率的指標，地下水位決定瞭泥炭堆積的潛在有效可容納空間。
거국내외근해함매암계층서지층학연구성과，운용기준면정현식변화화형정니탄퇴적속솔，도해불동가용납공간조건하니탄퇴적특정，인위가용납공간여니탄퇴적상호작용결정니탄퇴적화종지시간점、니탄퇴적지속시단급유리시기，이론상，임하체계역도유형성구역엄범분포매층적가능。기후조건시형량니탄생장속솔적지표，지하수위결정료니탄퇴적적잠재유효가용납공간。
Abatract:According to analyses of these previous Chinese and worldwide study results with respect to sequence stra-tigraphy of paralic coal-bearing strata,the sinusoidal base-level and invariable rates of peat accumulation, we illustrate the characteristics of peat accumulation under different rates of accommodation,which reveals that the interplay between accommodation and peat accumulation determines the times of accumulating and terminating peat and duration and pref-erable time of peat accumulation.Hence,the regionally extensive coal seams may occur in any system tracts for theoreti-cal analyses.Climate is a very important factor for evaluating rate of peat production and the groundwater table deter-mines the potential accommodation for peat accumulation.
