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101.
由于缺乏早期资料,设计早期油气田(藏)开发方案是非常困难的。在制作翁氏模型的Qctm/No-ER图版和ER-ctR图版过程提出根据探明储量No、经济极限产量Qc、假定达到峰值产量的时间tm、最终采收率ER,由翁氏模型的Qctm/No-ER图版求取增长指数b,由翁氏模型ER-ctR图版求取ctR,再求出其他参数及所有的油气田(藏)开发指标,完成早期油气田(藏)开发方案设计。 相似文献
102.
Archaeological investigations in Camels Back Cave, western Utah, recovered a series of small-mammal bone assemblages from stratified deposits dating between ca. 12,000 and 500 14C yr B.P. The cave's early Holocene fauna includes a number of species adapted to montane or mesic habitats containing grasses and/or sagebrush (e.g., Lepus townsendii, Marmota flaviventris, Reithrodontomys megalotis, and Brachylagus idahoensis) which suggest that the region was relatively cool and moist until after 8800 14C yr B.P. Between ca. 8600 and 8100 14C yr B.P. these mammals became locally extinct, taxonomic diversity declined, and there was an increase in species well-adapted to xeric, low-elevation habitats, including ground squirrels, Lepus californicus and Neotoma lepida. The early small-mammal record from Camels Back Cave is similar to the 11,300–6000 14C yr B.P. mammalian sequence from Homestead Cave, northwestern Utah, and provides corroborative data on Bonneville Basin paleoenvironments and mammalian responses to middle Holocene desertification. 相似文献
103.
Raman spectra of diopside were collected from atmospheric pressure to 71 GPa. The pressure dependences of 22 modes were determined.
Changes occurred in the spectra at three different pressures. First, at approximately 10 GPa, the two Raman modes at 356 and
875 cm−1 disappeared, while the mode at 324 cm−1 split into two modes, diverging at this pressure with significantly different pressure shifts; second, at approximately 15
GPa, a small (1 to 2 cm−1) drop in several of the frequencies was observed accompanied by changes in the pressure dependency of some of the modes;
and third, above 55 GPa, the modes characteristic of chains of tetrahedrally coordinated silicon disappeared, while those
for octahedrally coordinated silicon appeared. The first change at 10 GPa appears to be a C2/c to C2/c transition involving a change in the Ca coordination. The third change above 55 GPa appears to be a change in the silicon
coordination. At 15 GPa, it is suggested that a change in compressional mechanism takes place.
Received: 14 November 2000 / Accepted: 9 January 2002 相似文献
104.
105.
X线侧位片与高分辨率CT对鼻骨骨折的对比研究 总被引:17,自引:0,他引:17
目的 通过86例鼻骨骨折的鼻骨X线侧位片与高分辨率CT(HRCT)对比研究,确定HRCT检查对鼻骨骨折的诊断价值。材料与方祛 86例鼻外伤或/和He、面外伤的患者均进行了鼻骨X线侧位摄影、HRCT扫描检查,经集体讨论,由有经验的放射医师对全部影像资料进行分析并进行统计学处理。结果HRCT显示所有的86例鼻骨骨折,但在此86例骨折中X线平片只显示了35例阳性,包括15例鼻骨汇合部骨折,7例双侧鼻骨骨折,3例复合骨折(鼻骨汇合部及双侧鼻骨骨折),l0例鼻区骨折。X线平片显示5l例为阴性。结论 对鼻骨骨折的诊断,HRCT明显优于鼻骨X线侧位片,HRCT扫描检查可提高X线隐性鼻骨骨折的诊断,并可明确鼻骨骨折的类型、范围和程度,为临床诊断和治疗提供可靠的依据。 相似文献
106.
107.
中国西南及邻区上地幔P波三维速度结构/ 总被引:8,自引:0,他引:8
利用ISC报告以及中国和NEIC基本测震台网报告中的80974条P波初至到时资料(地震数为7053,台站数为165,且地震和台站都分布在研究区内),对中国西南及邻区(北纬10~36、东经70~110)的深至400km的上地幔三维速度结构进行了研究,分辨率达22.初步结果表明:①研究区速度的横向不均匀性,虽随深度增加而减弱,但至400km深度时仍很明显;②在北纬16和24的纵剖面上,可以看到与印度板块向东和欧亚板块相碰撞挤压相对应的速度结构,以及印度板块与欧亚板块速度结构的差异.在东经90的纵剖面上,与印度板块向北俯冲到欧亚板块(青藏高原)之下相对应的速度结构也比较明显;③在90km深度的横剖面上,由缅甸的密支那至越南的洞海的低速条带,可能与红河断裂带有关;④ 提出并使用了能够更为准确直观地描述分辨率好坏的图示方法. 相似文献
108.
关于绝对重力仪的发展和我们的思考 总被引:1,自引:3,他引:1
介绍了近年来出现的新型绝对重力仪,认为该仪器是控制地球重力场信息的重要工具,特别对FG5型的如何改进及我国绝对重力仪的如何发展,提出了建议。 相似文献
109.
110.
Meretta Lake (Resolute Bay, Cornwallis Island, Nunavut, Canada) is a high arctic lake that received raw sewage for almost 50 years from the Canadian Department of Transport Base. The lake was sampled from 1968–72 during the International Biological Programme, as part of the Char Lake Project. As the number of users at the Transport Base declined throughout the 1990s, so too did the lake's nutrient levels, and Meretta Lake is now classified as oligotrophic. A previous diatom-based paleolimnological study revealed marked species assemblage shifts coincident with sewage inputs beginning in the late 1940s; however, because the core was taken at a time when nutrient levels were still relatively high (i.e., 1993), the diatom record did not yet track any signs of recovery. In this present study, we examined fossil diatom assemblages from a sediment core taken in 2001. Our results indicate a shift to the pre-impact diatom assemblages in the most recent sediments, indicating that the paleolimnological record is tracking the decreased nutrient inputs to this high arctic lake, and confirms that no significant lags exist in these largely ice-covered lakes. 相似文献