lenticular hypermetropia
1.FLASER—LENTICULAR BEDDINGS IN CARBONATE ROCKS OF THE UPPER PRECAMBRIAN GAOYUZHUANG FORMATION IN THE MING TOMBS AREA,BEIJING
2.To optimize the design of lenticular stereoscopic LCD,the optical software ASAP(Advanced System Analysis Program)is used to model and simulate.
3.The dark-gray traction current deposits belong to internal-tide deposits, it develops sandstones and siltsands, and charactered with lenticular, wave, flaser bedding, bimodal cross-bedding and ripple mark.
4.Results Symmetric long T_1 and T_2 signals were found in central pontine region,lenticular nucleus,caudate nucleus,and thalamus. CE MRI showed no apparent enhanced lesions.
5.The deposit occurs in the sandstone?conglomerates of Anyuan Group in the upper Triassic,controled by NE?strike faults. The Orebodies are layer like or lenticular,changing with the folding of the strata. The grade of Cobalt ranges from 0.024%-1.15%,averaging at 0.4028%.
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7.The Yankou Formation in the Upper Ordovician of Tonglu County in Zhejiang Province consists mainly of rhythmically thin alternating layers of gray fine-grained sandstones, siltstones and dark-gray mudstones, silty mudstones, in which the typical flaser, wavy, lenticular bedding and rhythmic stratification are well developed, with 2-3 intercalated beds of gray medium- to thick-bedded conglomerates in the base of the formation.
8.Analysis of petroleum geology, reservoir types and distribution in Lujiapu Depression indicates that: the forming and distribution of reservoirs had been controlled by source area, source-reservoir relationship, petrophysical characteristics, sedimentary facies and secondary structure , and oil is most abundant in reservoirs around hydrocarbon kitchen; the upper member of Jiufutang formation which was entrained or embedded in the main oil source layer has well developed reservoir and good petrophysical property and is the principle oil-bearing interval; the mid-fan and fan delta front of nearshore submarine fan is the most favorite facies; the steep slope of the depression mainly consists of structural reservoirs, the slope belt mainly consists of structural-lithologic and updip pinchout reservoirs, the depressed belt mainly consists of lenticular lithologic reservoirs.
