later periods

later periods的基本解释

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后代

与later periods相关的网络例句 [注：此内容来源于网络，仅供参考]

E. , approximately four months; 2 the active periods occur much longer than the non-active periods; the main climatic characteristics of the non-active periods, compared with the active periods, is weaker monsoon with westerlies at 850-hPa and easterlies at 200-hPa on the deviation fields of circulations over the SCS (active time minus non-active time); it is warmer in the active periods than in the non-active periods at lower and upper levels; 3 in most circumstances, the low frequency vibrations of the summer monsoon and its rainfall are quite in phase.

2其中活跃期出现时间要比非活跃期长的多。与活跃期相比非活跃期主要气候特征表现为季风的减弱，在环流的偏差场上在南海上空850hPa上为西风，200hPa上为东风，活跃期高低空都比非活跃期要暖一些。(3)在多数情况下夏季风和夏季风降水的30-60天的低频振荡比较一致。

White snow tower' under 16h light/d flowered 13d earlier and ended 13d later than that under nature light,'White snow tower' under 14h light/d flowered 20d later and ended 14d later than CK;'White-red peony' under 12h light/d flowered 1d earlier and ended 10d later than CK,'White-red peony' under 14h light/d flowered 1d later and ended 10d later than CK, the blooming date of plants under 16h light/d was the same as CK, but ended 31d later than CK.

在花期方面，&白雪塔&在16小时的光照条件下可提前13天开花、而末花期推迟13天，14小时的光照处理推迟20天开花，末花期推迟14天；&花牡丹&12小时处理下开花时间只比CK提前一天，14小时处理推迟一天，16小时处理与CK同天开放，不过各长日照处理末花期都不同程度延后，16小时、14小时、12小时光照处理的末花期分别比CK晚了31天、10天、10天。

The Lower/Upper Cretaceous boundary in Songliao Basin is,therefore,between the Quantou and Denglouku formations,instead of between the Quantou and Qingshankou formations.2.The dark mudstones and shales in the Member 1 of Qingshankou Formation are of high organic carbon and low diasteranes contents.Organic geochemical characters are illustrated by biomarkers of 28,30-bisnorhopane and gammacerane,and positive excursion of kerogen isotopes.It is suggested that the dark mudstones and shales in the Member 1 of Qingshankou Formation are the products of lake anoxic period.It corresponds to the oceanic anoxic event at Cenomanian-Turonian boundary in Cretaceous.3.Based on the study of biostratigraphy,chronostratigraphy,magnetostratigraphy and event stratigraphy,a correlation of the lacustrine sequence to marine standard has been proposed,i.e.,the Quantou Formation corresponds to Cenomanian stage,Qingshankou Formation correlates to Later Cenomanian-Early Turonian,Yaojia Formation to Later Turonian-Coniacian,Nenjiang Formation to Santonian-Campanian.Sifangtai and Minshui Formations to Maastrichtian. 4.Analysis of lithology,lithofacies and microfossils of Cretaceous in Songliao Basin, shows that shore and shallow lake facies yield the most abundant microfossil groups,and the predelta and deltaic distributary plain facies rich in fossils as well.In the shore and shallow lake areas during the high level periods(such as Qingshankou and Nenjiang sedimentary periods),the lacustrine biota are of high diversity and high abundance.

因此，松辽盆地上、下白垩统的界线应在泉头组的底界，即泉头组与登娄库组之间，而不是泉头组的顶界。2、青山口组一段黑色泥岩、页岩具有有机碳含量高、重排甾烷含量低，生物标志物出现28，30—双降藿烷和伽马蜡烷，干酷根碳同位素具有正向偏移等有机地球化学特征，表征为青山口组一段黑色页岩、油页岩是古湖泊缺氧事件的产物，它对应于白垩纪古海洋Cenomanian—Turonian期界线附近缺氧事件，二者具同步性。3、通过生物地层学、年代地层学、磁性地层学和事件地层学研究，认为泉头阶大体相当于Cenomanian阶，青山口阶相当于晚Cenomanian—早Turonian阶，姚家阶对应于晚Turonian—Coniacian阶，嫩江阶对应于Santonian—Campanian阶，四方台阶和明水阶相当于Maastrichtian阶。4、通过对松辽盆地上白垩统的岩性、岩相及微体化石分析，认为滨浅湖相是微体生物群最为发育的相带，其次为三角洲前缘相和三角洲分流平原相。

与later periods相关的网络解释 [注：此内容来源于网络，仅供参考]

no later than：不迟于//later on 以后,后来

sooner or later 迟早/See you later! 再见! | no later than 不迟于/later on 以后,后来 | soon ad. 不久,马上

Perioperative periods：围术期

近代:the late periods | 围术期:Perioperative periods | 多时期:multiple periods

menarche ; onset of menses：初潮

月经 menstruation ; menses ; periods ; menstrual periods | 初潮 menarche ; onset of menses | 停经 menopause