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161.
胶莱盆地东缘早白垩世早期莱阳群沉积体现了湖盆由开始形成—鼎盛—萎缩消亡的全过程,发育由冲洪积相—湖相—三角洲相—河流相沉积的完整序列,且由东至西,由湖相到河流相逐渐过渡;古水流方向显示莱阳期盆地中心位于朱吴断裂、海阳断裂带之间,以断裂带为界,以西水流方向大致为由NW至SE向,以东水流方向则为由SE至NW向;早白垩世早期莱阳期盆地的形成与演化明显受区域性牟(平)-即(墨)断裂带活动所控制。 相似文献
162.
Miquel Poyatos‐Mor George D. Jones Rufus L. Brunt Daniel E. Tek David M. Hodgson Stephen S. Flint 《Basin Research》2019,31(5):920-947
Exhumed basin margin‐scale clinothems provide important archives for understanding process interactions and reconstructing the physiography of sedimentary basins. However, studies of coeval shelf through slope to basin‐floor deposits are rarely documented, mainly due to outcrop or subsurface dataset limitations. Unit G from the Laingsburg depocentre (Karoo Basin, South Africa) is a rare example of a complete basin margin scale clinothem (>60 km long, 200 m‐high), with >10 km of depositional strike control, which allows a quasi‐3D study of a preserved shelf‐slope‐basin floor transition over a ca. 1,200 km2 area. Sand‐prone, wave‐influenced topset deposits close to the shelf‐edge rollover zone can be physically mapped down dip for ca. 10 km as they thicken and transition into heterolithic foreset/slope deposits. These deposits progressively fine and thin over tens of km farther down dip into sand‐starved bottomset/basin‐floor deposits. Only a few km along strike, the coeval foreset/slope deposits are bypass‐dominated with incisional features interpreted as minor slope conduits/gullies. The margin here is steeper, more channelized and records a stepped profile with evidence of sand‐filled intraslope topography, a preserved base‐of‐slope transition zone and sand‐rich bottomset/basin‐floor deposits. Unit G is interpreted as part of a composite depositional sequence that records a change in basin margin style from an underlying incised slope with large sand‐rich basin‐floor fans to an overlying accretion‐dominated shelf with limited sand supply to the slope and basin floor. The change in margin style is accompanied with decreased clinoform height/slope and increased shelf width. This is interpreted to reflect a transition in subsidence style from regional sag, driven by dynamic topography/inherited basement configuration, to early foreland basin flexural loading. Results of this study caution against reconstructing basin margin successions from partial datasets without accounting for temporal and spatial physiographic changes, with potential implications on predictive basin evolution models. 相似文献
163.
南大西洋两岸盆地海相烃源岩特征与控制因素 总被引:1,自引:0,他引:1
南大西洋两岸盆地漂移期层系油气资源十分丰富,通过对两岸重点盆地漂移期主力烃源岩发育层位、生烃潜力、识别特征和分布范围对比分析,明确两岸发育早、晚两套主力海相烃源岩。其中,晚期的赛诺曼-土仑阶海相烃源岩分布范围较广。整体上,两岸北段和赤道段盆地漂移期主力烃源岩地化指标优于中段和南段盆地,西非一侧海域盆地烃源岩地化指标优于南美一侧盆地。在对重点钻井的矿物元素化验分析、沉积相和古地理分析基础之上,总结了局限海湾的古地理背景和沉积相带类型控制优质海相烃源岩发育程度和分布范围的规律,并进一步指出南大西洋两岸北段和赤道段盆地漂移期成熟生烃灶平面分布范围内的深水沉积砂体是主要有利勘探方向,以找油为主,中段含盐盆地内紧邻盐微盆的漂移期深水沉积砂体勘探潜力次之。 相似文献
164.
The northeastern shelf margin of the South China Sea(SCS) is characterized by the development of large scale foresets complexes since Quaternary. Based on integral analysis of the seismic, well logging and paleontological data, successions since ~3.0 Ma can be defined as one composite sequence, consist of a set of regional transgressive to regressive sequences. They can be further divided into six 3 rd order sequences(SQ0–SQ5) based on the Exxon sequence stratigraphic model. Since ~1.6 Ma, five sets of deltaic systems characterized by development of wedge-shaped foresets complexes or clinoforms had been identified. High-resolution seismic data and the thick foresets allowed further divided of sub-depositional sequences(4 th order) of regression to transgression, which is basically consistent with published stacked benthic foram O-isotope records. Depositional systems identified in the study area include deltaic deposits(inner-shelf deltas and shelf-edge deltas), incised valleys, and slope slumping massive deposits. Since ~1.6 Ma, clinoforms prograded from the southern Panyu Lower Uplift toward the northern Baiyun Depression, shelf slope break migrated seaward, whereas the shelf edge of SQ0 migrated landward. The development of incised valleys in the continental shelf increased upward,especially intensive on the SB3 and SB2. The slumping massive deposits increased abruptly since SB2, which corresponds to the development of incised valleys. The evolution of depositional systems of continental slope mainly controlled by the combined influence of sea level changes, tectonic movements, sediment supply and climate changes. Since ~3.0 Ma, relative sea level of the northern SCS had been experienced transgression(~3.0 Ma BP) to regression(~1.6 Ma BP). The regional regression and maximum transgressions of the composite sequences were apparently enhanced by uplift or subsidence related to tectono-thermal events. In addition,climatic variations including monsoon intensification and the mid-Pleistocene transition may have enhanced sediment supply by increasing erosion rate and have an indispensable influence on the development of the incised valleys and 5 sets of deltaic systems since ~1.6 Ma. 相似文献
165.
本文以二倍体和三倍体虹鳟(Oncorhynchus mykiss)幼鱼为实验对象,探究急性高温胁迫下,不同倍性虹鳟热休克蛋白家族(hsps)基因表达水平。选取二倍体和三倍体虹鳟幼鱼,分别进行常温处理(14℃)和高温胁迫(22℃),并在高温胁迫48h后,将虹鳟置于常温(14℃)恢复48h。分别在实验开始的0,12,24,48,72和96h进行取样,测定实验虹鳟肝脏和肌肉组织中的hsp70s(hsp70a,hsp70b),hsp90s (hsp90a1a,hsp90a2a,hsp90a1b,hsp90a2a,hsp90b1,hsp90b2)mRNA水平。结果表明:hsp70s和hsp90s的各个亚型均能对热胁迫做出反应,并具有应答幅度的组织特异性和时间特异性。在胁迫6和24h后,上述基因mRNA水平达到最高,随后降低。三倍体幼鱼肝脏和肌肉hsps mRNA表达水平的峰值显著高于二倍体幼鱼。研究结果显示,三倍体虹鳟对高温环境更为敏感,需要消耗更多的能量用于适应高温环境。 相似文献
166.
宇宙线的起源是高能天体物理的核心问题之一.一直以来,超新星爆发被认为是能谱膝区以下宇宙线的主要来源.多波段观测表明,超新星遗迹有能力加速带电粒子至亚PeV (10~(15)eV)能量.扩散激波加速被认为是最有效的天体高能粒子加速机制之一,而超新星遗迹的大尺度激波正好为这一机制提供平台.近年来,一系列较高精度的地面和空间实验极大地推动了对宇宙线以及超新星遗迹的研究.新的观测事实挑战着传统的扩散激波加速模型以及其在银河系宇宙线超新星遗迹起源学说上的应用,深化了人们对宇宙高能现象的认识.结合超新星遗迹辐射能谱的时间演化特性,构建的时间依赖的超新星遗迹粒子加速模型,不仅能够解释200 GV附近宇宙线的能谱反常,还自然地形成能谱膝区,甚至可以将超新星遗迹粒子加速对宇宙线能谱的贡献延伸至踝区.该模型预期超新星遗迹中粒子的输运行为表现为湍流扩散,这需要未来的观测以及与粒子输运相关的等离子体数值模拟工作来进一步验证. 相似文献
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170.
三株赤潮硅藻5.8S rDNA及转录间隔区(ITS)的克隆及序列分析 总被引:1,自引:1,他引:0
对引发赤潮的3株硅藻——1株尖刺拟菱形藻(Pseudo-nitzshia pungens)和2株中肋骨条藻(Skeletonema costatum)的5.8SrDNA和ITS(internal transcribed spacers)序列进行了PCR扩增、克隆和序列测定,并分析了硅藻门10株赤潮藻(7株从GenBank获得)的系统进化关系.研究结果表明,尖刺拟菱形藻的ITS和5.8SrDNA的长度为693bp,SK-1(分离自东海赤潮暴发区)测序得到715bp,除ITS和5.8SrDNA外,还包含部分18SrDNA和28SrDNA;SK-2(分离自青岛养殖场)的ITS和5.8SrDNA的长度为331bp,尖刺拟菱形藻与从GenBank中获得的2株尖刺拟菱形藻相似程度最高,为100%,与该属的多列拟菱形藻相似程度稍低,为82.9%.SK-2的ITS序列与SK-1的相似程度很低,只有51%,但与拟中肋骨条藻的ITS序列相似程度高,为95.5%.SK-1的ITS序列与拟中肋骨条藻的相似程度也低,为56.7%.系统进化树反映的结果与相似性反映的结果一致.研究的该株尖刺拟菱形藻从根据ITS序列研究的结果与形态鉴定的结果看是一致的;SK-2可能属于拟中肋骨条藻;SK-1比较特殊,有待于用其他的方法进一步研究确定其分类地位. 相似文献