数字观测仪器机房保温措施     

白琪光  杨玉光  战晓芳 《东北地震研究》2002,18(3):42-45

介绍了朝阳地震台根据公皋井的实际情况，按照《规范》对前兆数字仪器设备工作环境的要求所采取的机房防寒保温的方法和措施。  相似文献   

Seismic facies analysis of Westphalian sequences of the southern North Sea     

David J. Evans  Alan Meneilly  Gordon Brown 《Marine and Petroleum Geology》1992,9(6)

Differing seismic facies are observed from within the Westphalian sequences of the southern North Sea. A review of published synthetic seismograms and seismic data from known coal-bearing basins establishes seismic facies types and their relationships. Similar reflection character is recognized from Westphalian sequences in the southern North Sea and lithologies confirmed by borehole information. Probable sand/silt or clastic-prone Upper Coal Measures (Westphalian C/D) stages and coal-prone Lower and Middle Coal Measures (Westphalian A, B and part C) stages can be defined and mapped, providing information on the regional distribution of source and reservoir rocks and stratigraphic plays. It is suggested that sand-prone channel complexes or clastic dominated areas within the mainly A/B stages can be recognized and mapped, providing information on migration pathways and stratigraphic plays.  相似文献   

鲁西北平原可持续农业发展的机制与途径——以东昌府区为例   总被引：1，自引：1，他引：0  

王云才 《地理科学》2000,20(4):342-349

以鲁西北平原东昌府区为典型案例,通过动态分析和典型调查,揭示东昌府区农业可持续发展的投入机制、市场机制、科技应用、经营管理和决策调控机制的运行规律。在此基础上,针对性提出了农业可持续发展的产业结构调整;农业市场化、企业化和专业化基地发展,推动农业产业化进程;发展农业科技,提高农民素质,加强农业人力资本建设和建立农业可持续发展的调控机制四个方面的发展对策。  相似文献   

临清市地下水漏斗区与地面沉降研究     

周玉红  王颖  李洋 《地下水》2009,31(3):38-40,71

随着经济的发展和人口的不断增加,城区用水量大幅度上升.临清市城区生活及工业用水全部为地下水,由于大量超采地下水,造成了地下水位埋深大幅度下降,形成了以城区为中心的大面积地下水漏斗区.地下水位大幅度下降,势必引起地面沉降等环境地质问题.因此摸清临清城区地下水的下降规律及地质状况、漏斗区的范围、地面沉降的状况并提出阻止地面沉降的措施,对地上建筑物、地下构筑物保护等都具有十分重要的意义.  相似文献   

厦门干旱成因和防旱抗旱对策     

卢海新  朱天赐 《气象研究与应用》2010,31(3)

通过对厦门市历史旱情分析,找出干旱原因,提出防旱抗早对策。  相似文献   

广西合浦包墩水库工程地质问题分析及对策     

梁永玖 《云南地质》2011,30(1):112-114

对包墩水库建成运行以来的工程地质、水文地质及大坝渗漏、稳定作出评价,归纳存在的工程地质问题,提出相应的防渗漏处理措施。  相似文献   

Geology and mining practice in relation to shallow subsidence in the Northern Coalfield,New South Wales     

G. H. McNally 《Australian Journal of Earth Sciences》2013,60(1):21-34

The former Northern Coalfield, comprising much of the Newcastle‐Maitland‐Cessnock‐Lake Macquarie region, has now been mined for two hundred years. Most of the twenty‐odd seams in the Newcastle, Tomago and Greta Coal Measures have been worked, but the bulk of production has been drawn from just four coalbeds: the Borehole, Greta, Homeville and Great Northern Seams. Literally hundreds of mine names are on record for the coalfield, the great majority working these seams at depths of less than 30 m. This paper reviews regional subsidence problems in the context of mining history, past mining practices and coal measures geology. Subsidence over shallow bord‐and‐pillar workings may result in highly disturbed ground, open fissures, cratering, seam fires and ‘creeps’ (slow surface movements caused by gradual closure of mine cavities). This form of subsidence differs from that over modern longwall mines in being less predictable, affecting much smaller areas, and occurring sometimes decades after mine abandonment. The geological factors contributing to this subsidence hazard include the multiplicity of seams, the strong roof sandstones, stiff coal and relatively soft floors, and the presence of faults and dykes. The working of thick seams like the Borehole Coal in up to three phases, leaving high, slender pillars, also contributed to later ground instability. Contrary to expectation, the main problem areas are not over haphazardly laid‐out convict‐era pits, but rather above small hand‐worked scavenger mines (‘ratholes’) which operated as late as the 1950s. Many of these short‐lived collieries still contain large voids at shallow depth, sometimes only a few metres, which must eventually collapse or be backfilled.  相似文献   

Alternating episodes of extension and contraction during the Triassic: evidence from Mesozoic sedimentary basins in eastern Australia     

A. Babaahmadi  G. Rosenbaum  J. Esterle 《Australian Journal of Earth Sciences》2013,60(5):563-579

Triassic to Lower Cretaceous continental sedimentary basins occur in eastern Australia, but the tectonic and structural evolution of these basins is not fully understood. Using gridded aeromagnetic data, seismic reflection data and field observations, we conducted a structural analysis aimed at characterising major faults and deformation style in these sedimentary basins. Our results show evidence for two alternating episodes of rifting during the Triassic. An earlier episode of rifting, which took place in the Early Triassic to early Late Triassic, is inferred based on synsedimentary normal faults in the Nymboida Coal Measures and the boundary West Ipswich Fault System in the Esk Trough. This phase of rifting was followed by a contractional event that resulted in tilting, folding, and thrust faulting. Evidence of synsedimentary normal faults and bimodal volcanism indicates that another rifting phase occurred during the Late Triassic and resulted in the development of the Ipswich Basin. From the latest Late Triassic to the Early Cretaceous, the accumulation of continental sediments in the Clarence-Moreton Basin was accompanied by subsidence. We suggest that the alternating rifting episodes and contraction were ultimately controlled by plate boundary migration and switches between trench retreat and advance during the Triassic.  相似文献   

Age of the Yarrabee and accessory tuffs: implications for the upper Permian sediment-accumulation rates across the Bowen Basin   总被引：1，自引：1，他引：0  

S. A. Ayaz  M. Martin  J. Esterle  Y. Amelin  R. S. Nicoll 《Australian Journal of Earth Sciences》2016,63(7):843-856

The Yarrabee Tuff is a stratigraphically significant marker across the Bowen Basin separating the Fort Cooper–Burngrove–Fair Hill formations from the overlying Rangal and equivalent coal measures. At least three to four persistent tuffs (referred here as accessary tuffs) beneath the Yarrabee Tuff were recognised in the Fort Cooper Coal Measures as suitable for regional stratigraphic correlations. In this study, we determined the ages of the Yarrabee and accessary tuffs across different morphotectonic zones of the basin through high-precision U–Pb dating of zircon with the CA-IDTIMS technique. The age of the Yarrabee Tuff is found to be 252.69 ± 0.16 Ma in the Duckworth 11 well, 253.07 ± 0.22 Ma in the Crocker Gully 2 well and <252.58 ± 0.23 Ma in the Peat 1 well. The age range of the Yarrabee Tuff coincides with the previously published date of the Kaloola Tuff Member in Meeleebee 5 suggesting that the tuffs are stratigraphically equivalent. The age range for the accessory tuff 1 is 253.12 ± 0.12 Ma to 252.85 ± 0.16 Ma, 253.45 ± 0.08 Ma for accessory tuff 2 and 253.77 ± 0.17 Ma to 253.57± 0.18 Ma for accessory tuff 3, placing them in the upper Changhsingian Stage. The age of the accessory tuff 6 (less laterally consistent in the basin) from the Fair Hill Formation is 254.03 ± 0.03 Ma, placing it in the lower Changhsingian Stage. The age-constrained intervals allow the estimation of sedimentation rates using decompacted coal and clastic sediment thickness. In the Taroom Trough, the temporal variation in sedimentation rates is found to be 902 m/Ma in the Fair Hill Formation decreasing to 234.5 m/Ma in the overlying Burngrove Formation, reflecting a decrease in accommodation or sediment supply upwards in the sequence. Across the basin, the sedimentation rates for the Burngrove Formation are consistently higher in the Taroom Trough ranging between 234.5 and 224.5 m/Ma and lower rates of 112 m/Ma in the Roma Shelf. This regional variation reflects areas of high sedimentation rates that are high accommodation sites recognised by split coal seams and increased interburden. Conversely, low sedimentation rates reflect low accommodation sites, such as the Roma Shelf and the Burunga Anticline that are characterised by coalesced coal seams. The results help to understand stratal relationships across variable accommodation sites, basin-fill history of the basin including extent of sediment supply and paleotopographic controls during the evolution of the Bowen Basin. We also discuss criteria for interpreting the results of CA-IDTIMS U–Pb dating and consider the possible geological uncertainties related to either the primary magmatic processes or secondary reworking of tuffs at the site of deposition.  相似文献   

A relation between abrasiveness and quartz content for some Coal Measures sediments     

G. West 《Geotechnical and Geological Engineering》1986,4(1):73-78

Conclusions 1. For a limited range of Coal Measures sediments, it has been shown that a good relation exists between the abrasiveness of the rocks and their quartz content.2. In this instance it was not possible to make any correlation with cutter wear, but it would be expected from the above result that the higher the quartz content of the rock the greater would be the wear on the cutters.  相似文献