桂西北上二叠统及下三叠统古岩溶不整合

文章描述了桂西北乐业、天峨等地区发现于上二叠统顶部、下三叠统顶部的 2个古岩溶不整合面 ,及其暴露、沉积间断特征 ,分析了它们的形成时代。通过这 2个I型层序界面的确认 ,讨论了其与地层划分对比、沉积环境及盆地分析、断裂的发育及与微粒型金矿的关系与意义。     

Sedimentology and stratigraphy of a transgressive, muddy gravel beach: Waterside Beach, Bay of Fundy, Canada

Sediments exposed at low tide on the transgressive, hypertidal (>6 m tidal range) Waterside Beach, New Brunswick, Canada permit the scrutiny of sedimentary structures and textures that develop at water depths equivalent to the upper and lower shoreface. Waterside Beach sediments are grouped into eleven sedimentologically distinct deposits that represent three depositional environments: (1) sandy foreshore and shoreface; (2) tidal‐creek braid‐plain and delta; and, (3) wave‐formed gravel and sand bars, and associated deposits. The sandy foreshore and shoreface depositional environment encompasses the backshore; moderately dipping beachface; and a shallowly seaward‐dipping terrace of sandy middle and lower intertidal, and muddy sub‐tidal sediments. Intertidal sediments reworked and deposited by tidal creeks comprise the tidal‐creek braid plain and delta. Wave‐formed sand and gravel bars and associated deposits include: sediment sourced from low‐amplitude, unstable sand bars; gravel deposited from large (up to 5·5 m high, 800 m long), landward‐migrating gravel bars; and zones of mud deposition developed on the landward side of the gravel bars. The relationship between the gravel bars and mud deposits, and between mud‐laden sea water and beach gravels provides mechanisms for the deposition of mud beds, and muddy clast‐ and matrix‐supported conglomerates in ancient conglomeratic successions. Idealized sections are presented as analogues for ancient conglomerates deposited in transgressive systems. Where tidal creeks do not influence sedimentation on the beach, the preserved sequence consists of a gravel lag overlain by increasingly finer‐grained shoreface sediments. Conversely, where tidal creeks debouch onto the beach, erosion of the underlying salt marsh results in deposition of a thicker, more complex beach succession. The thickness of this package is controlled by tidal range, sedimentation rate, and rate of transgression. The tidal‐creek influenced succession comprises repeated sequences of: a thin mud bed overlain by muddy conglomerate, sandy conglomerate, a coarse lag, and capped by trough cross‐bedded sand and gravel.     

The sampling distribution of theW statistic of disjunction for the arbitrary division of a random rectangular distribution

The sampling distribution of the Wstatistic of disjunction has been estimated by Monte Carlo simulation for the case where the underlying distribution is a random rectangular (Poisson) variable that is divided into two groups at an arbitrary position. A transformation to sinh ^–1 log _e Wgave a variable that was acceptably normal, and from this a simple approximation for the distribution is given, together with a diagram of confidence limits of Wfor this case.     

Gravelly spit deposits in a transgressive systems tract: the Pleistocene Higashikanbe Gravel, central Japan

The Pleistocene Higashikanbe Gravel, which crops out along the Pacific coast of the Atsumi Peninsula, central Japan, consists of well‐sorted, pebble‐ to cobble‐size gravel beds with minor sand beds. The gravel includes large‐scale foreset beds (5–10 m high) and overlying subhorizontal beds (0·5–3 m thick), showing foreset and topset structure, from which the gravel has previously been interpreted as deposits of a Gilbert‐type delta. However, (1) the gravel beds lack evidence of fluvial activity, such as channels in the subhorizontal beds; (2) the foresets incline palaeolandwards; (3) the gravels fill a fluvially incised valley; and (4) the gravels overlie low‐energy deposits of a restricted environment, such as a bay or an estuary. The foresets generally dip towards the inferred palaeoshoreline, indicating landward accretion of gravel. Reconstruction of the palaeogeography of the peninsula indicates that the Higashikanbe Gravel was deposited as a spit similar to that developed at the western tip of the present Atsumi Peninsula, rather than as a delta. According to the new interpretation, the large‐scale foreset beds are deposits on the slopes of spit platforms and accreted in part to the sides of small islets that are fragments of the submerging spit during relative sea‐level rise. The subhorizontal beds include nearshore deposits on the spit platform topsets and deposits of gravel shoals or bars, which are reworked sediments of the spit beach gravels during a transgression. The lack of spit beach facies in the subhorizontal beds results from truncation by shoreface erosion. Dome structure, which is a cross‐sectional profile of a recurved gravel spit at its extreme point, and sandy tidal channel deposits deposited between the small islets were also identified in the Higashikanbe Gravel. The Higashikanbe Gravel fills a fluvially incised valley and occupies a significant part of a transgressive systems tract, suggesting that gravelly spits are likely to be well developed during transgressions. The large‐scale foreset beds and subhorizontal beds of gravelly spits in transgressive systems tracts contrast with the foreset and topset beds of deltas, characteristic of highstand, lowstand and shelf‐margin systems tracts.     

改进的地图制图点注记配置探测信息模型

点注记作为地图信息传输的媒介之一,是地图不可或缺的组成部分。以往对点注记的自动化配置研究主要考虑注记的冲突问题,忽略了背景要素的空间分布与结构特征,而背景要素分布结构与点注记质量密切相关。本文以注记清晰性、指代明确性、配置均匀性和归属正确性规则为出发点,构建点注记质量与背景要素的相关性量化描述,提出一种改进的探测信息模型。模型顾及了要素拓扑关系、数据结构、视觉位置、行政区划所导致的探测信息量的差异性,以国家1∶100万基础地理信息数据为例,将研究结果与第一代模型以及Maplex进行对比验证分析。试验表明,本文模型能够进一步减少局部区域的探测信息量,有效规避了背景要素,提升了注记的清晰性与可读性。     

Feeding habits and ontogenetic diet shifts of Bombay duck,Harpadon nehereus

Based on two bottom trawl surveys conducted in autumn 2000 and 2001, a total of 1106 stomach samples of Bombay duck Harpadon nehereus between 23–278 mm fork length were collected and analyzed. The results show that Bombay duck prey items consisted of 11 groups or 32 species, of which Apogon lineatus, Leptochela gracilis, Acetes chinensis, and Euphausia pacifi ca were the dominant prey species. Ontogenetic variations were found in feeding habits and feeding activity of Bombay duck. Feeding activity was highest in fi sh smaller than 50 mm, lowest in fi sh between 50 and 99 mm, and then increased with increasing size thereafter. As Bombay duck size increased, fi sh prey increased in importance, whereas euphausiids and decapods decreased in importance. Different trophic guilds were observed in feeding habits across the examined size range. Bombay duck smaller than 50 mm were zooplanktivores, mainly feeding on zooplankton and fi sh larva; those between 50 and 149 mm were generalist predators, mainly feeding on pelagic shrimps, demersal shrimps and fi shes; and those larger than 150 mm were piscivores, mainly feeding on fi shes.     

基于立体模型重叠度的航空摄影航线设计

针对地表起伏较大的山地或市区立体测图,提出一种基于立体模型重叠度的重叠度计算方案.与以往相比,它不计算相邻相片的实际重叠度,而是通过基于数字表面模型(DSM)计算相邻立体模型的实际重叠度来设计航线.试验表明,这一方案不仅能更好地满足立体测图对立体模型重叠度的要求,还能大幅减少相片和航线.     

三门湾海域主要底上动物生态位及种间联结性*

为探究三门湾海域物种间的资源利用情况及生态关系,在该海域进行了底拖网生物调查。根据2017年和2018年夏季在浙江省三门湾海域进行的大型底上生物研究结果,运用优势度(Y)、生态位宽度、生态位重叠、方差比率法(VR)、检验、联结系数(AC)、共同出现百分率(PC)对生态位和种间联结性进行了研究。结果表明:2017~2018年间三门湾海域共捕获大型底上动物53种,包括两年共有种,即主要底上动物22种。其中优势种3种,包括哈氏仿对虾(Mierspenaeopsis hardwickii)、中华栉孔虾虎鱼(Ctenotrypauchen chinensis) 和棒锥螺(Turritella terebra),这三个物种属中生态位种;三门湾主要底上动物依据生态位宽度值划分为3组,即广生态位种、中生态位种和窄生态位种;种对间生态位重叠值总体差异性较大,其与种对的食性、栖息环境密切相关;根据总体联结性分析得主要底上动物总体呈显著正关联,群落结构较为稳定; 检验、联结系数(AC)和共同出现百分率(PC)表明种对间联结性较弱,趋近于相互独立。三门湾大型底上动物的群落结构比较稳定,但种对间的关联性在逐渐下降。     

机载LiDAR旁向重叠区域冗余数据的消除算法

本文基于点云格网化的思想,提出了一种去除机载LiDAR航带间旁向重叠区域冗余数据的算法。该算法使用规则方格表示点云覆盖的区域,通过给网格赋值的方式提取重叠区域的冗余点云,最后删除靠近条带边缘的冗余点云。经过实验测试,该方法能够快速有效地去除重叠区的冗余数据;无需依赖航迹信息,因此也适用于地面激光点云的消冗。     

城市生态位测度研究——以天山北坡城市群为例

依据生态位理论,界定了城市生态位等相关概念。以天山北坡城市群为研究对象,选取1980-2010年人口、产业和投资等数据,根据城市生态位宽度模型、分异指数模型和重叠指数模型,分析了该城市群中各城市生态位空间宽度、生态位结构变化及其相互作用关系,为实现城市群的持续发展提供了新视角。结果表明：天山北坡城市群中,乌鲁木齐和石河子的人口生态位较大,而在经济生态位及资源生态位方面乌鲁木齐和克拉玛依位居前两位,说明城市生态位具有不连续性特征。天山北坡城市群中经济生态位宽度最大值的城市是最小值城市的32倍,说明天山北坡城市群中城市生态位宽度的差异悬殊。同时,天山北坡城市群的人口、经济及资源生态位分异指数均呈现下降趋势,人口与经济要素在空间上的不平衡得以改善,城市之间人口、经济发展的差距在逐渐缩小。天山北坡城市群正逐渐由“单中心”城市群向“多中心”城市群演进。在城市生态位重叠指数方面,城市之间的重叠指数呈现不断增大趋势,说明天山北坡城市之间的产业结构趋同性增强,同质竞争日趋激烈。针对天山北坡城市群城市生态位特征,按照专业化分工协作的要求,提出了城镇组团错位发展的设想。