推定歴年瞻禮日法Chui ding li nian zhan li ri fa.

Sur le calendrier ecclésiastique et le calcul des fêtes.Par divers Pères de la Compagnie de Jésus, non énumérés ; extraits par un lettré de Wu lin ; date de la dynastie des Ming.15 feuillets.

Sheng jiao ri ke.

Contient : I, livre 3Tian zhu ye su shou nan shi mo ; II, livre 3Xiang tian zhu fu song, etc ; III, livre 3Wu shang jing gui cheng ; IV, livre 3Song ; V, livre 3Shan zhong yi ying li dian

Chinois 7373

Contient : I天主教要Tian zhu jiao yao ; II聖號經Sheng hao jing ; 458天主經Tian zhu jing ; IV天神朝拜聖母經Tian shen chao bai sheng mu jing ; V信經Xin jing ; VI天主十誡Tian zhu shi jie

Chinois 7379

Contient : I ; II天主聖教小引Tian zhu sheng jiao xiao yin ; III聖夢歌Sheng meng ge ; IV推驗正道論Chui yan zheng dao lun ; V醒世問編Xing shi wen bian ; VI二十五言Er shi wu yan ; VII高士傳Gao shi zhuan ; VIII永福天衢Yong fu tian qu

聖教要訓Sheng jiao yao xun.

Contient : ISheng hao jing ; IITian zhu jing ; IIITian shen chao bai sheng mu jing ; IVXin jing ; VTian zhu shi jie ; VISheng jiao hui si gui ; VII天主事情問荅Tian zhu shi qing wen da ; VIII人讐有三Ren chou you san ; IX十誡問荅Shi jie wen da ; X悔罪問荅Hui zui wen da ; XIHui zui jing ; XII天學警言Tian xue jing yan

聖母領報會規Sheng mu ling bao hui gui.

Contient : I入會奉事聖母經Ru hui feng shi sheng mu jing ; II聖母領報會小引Sheng mu ling bao hui xiao yin ; III規條Gui tiao ; IV聖母領報會大赦規條Sheng mu ling bao hui da sha gui tiao ; V入會禮儀Ru hui li yi

Chinois 7420

Contient : I聖教啟蒙指要Sheng jiao qi meng zhi yao ; IIJiang ling sheng shui wen da ; III五傷聖方濟各禱文Wu shang sheng fang ji ge dao wen ; IV聖伯多祿亞甘太辣祝文Sheng bai duo lu ya gan tai la zhu wen ; V聖人文度辣讚聖人安多尼祝文Sheng ren wen du la zan sheng ren an duo ni zhu wen ; VI聖若瑟七苦七樂文Sheng ruo se qi ku qi luo wen

聖教切要Sheng jiao qie yao.

Contient : I聖號經 。天主經 。聖母經 。信經。Sheng hao jing. Tian zhu jing. Sheng mu jing. Xin jing ; II天主十誡Tian zhu shi jie ; III聖教四規Sheng jiao si gui ; IV聖事之迹Sheng shi zhi ji ; V同性 (sic) 外親四代之圖Tong xing wai qin si dai zhi tu

天主聖教永瞻禮單

voir Chinois 7276, article XII.Tian zhu sheng jiao yong zhan li dan.Calendrier perpétuel des fêtes de la religion chrétienne.Par le P. Couplet ; copie faite (1712) par An dang, de Wu lin. Au début, frontispice représentant la croix tombale de Candide Xu, morte en 1680, fille de Xu Guang qi.85 feuillets.

進善錄Jin shan lu.

Contient : I認識本義Ren shi ben yi ; II約同眾禱Yue tong zhong dao ; III默想神功Mo xiang shen gong ; IV力行警語Li xing jing yu ; V領聖體功課Ling sheng ti gong ke ; VI神領聖體經Shen ling sheng ti jing ; VII領聖體問荅Ling sheng ti wen da ; VIII各種赦條Ge zhong sha tiao ; IX祈禱神功Qi dao shen gong ; X通功神課Tong gong shen ke ; XI付洗幼孩規說Fu xi you hai gui shuo

聖事問荅Sheng shi wen da.

Contient : I聖號經Sheng hao jing ; II天主經Tian zhu jing ; III聖母經Sheng mu jing ; IV信經Xin jing ; V天主十誡Tian zhu shi jie ; VI悔罪經Hui zui jing ; VII要理問荅Yao li wen da ; VIII告解要理Gao jie yao li ; IX聖體問荅Sheng ti wen da ; X-XVIII

Chinois 7451

Contient : I天主聖經經文Tian zhu sheng jiao jing wen ; IITian zhu shi jie ; III聖教四規Sheng jiao si gui ; IV天主教要問荅Tian zhu jiao yao wen da

Structural, stratigraphic and geochemical studies of the Horwood Peninsula - Gander Bay Area, Northeast Newfoundland /

The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.

Sample preparation and heavy metal determination by atomic spectrometry /

Microwave digestions of mercury in Standards Reference Material (SRM) coal samples with nitric acid and hydrogen peroxide in quartz vessels were compared with Teflon® vessel digestion by using flow injection cold vapor atomic absorption spectrometry. Teflon® vessels gave poor reproducibiUty and tended to deliver high values, while the digestion results from quartz vessel show good agreement with certificate values and better standard deviations. Trace level elements (Ag, Ba, Cd, Cr, Co, Cu, Fe, Mg, Mn, Mo, Pb, Sn, Ti, V and Zn) in used oil and residual oil samples were determined by inductively coupled plasma-optical emission spectrometry. Different microwave digestion programs were developed for each sample and most of the results are in good agreement with certified values. The disagreement with values for Ag was due to the precipitation of Ag in sample; while Sn, V and Zn values had good recoveries from the spike test, which suggests that these certified values might need to be reconsidered. Gold, silver, copper, cadmium, cobalt, nickel and zinc were determined by continuous hydride generation inductively coupled plasma-optical emission spectrometry. The performance of two sample introduction systems: MSIS™ and gas-liquid separator were compared. Under the respective optimum conditions, MSIS^"^ showed better sensitivity and lower detection limits for Ag, Cd, Cu, Co and similar values for Au, Ni and Zn to those for the gas-liquid separator.

Bounds on edit metric codes with combinatorial DNA constraints

The design of a large and reliable DNA codeword library is a key problem in DNA based computing. DNA codes, namely sets of fixed length edit metric codewords over the alphabet {A, C, G, T}, satisfy certain combinatorial constraints with respect to biological and chemical restrictions of DNA strands. The primary constraints that we consider are the reverse--complement constraint and the fixed GC--content constraint, as well as the basic edit distance constraint between codewords. We focus on exploring the theory underlying DNA codes and discuss several approaches to searching for optimal DNA codes. We use Conway's lexicode algorithm and an exhaustive search algorithm to produce provably optimal DNA codes for codes with small parameter values. And a genetic algorithm is proposed to search for some sub--optimal DNA codes with relatively large parameter values, where we can consider their sizes as reasonable lower bounds of DNA codes. Furthermore, we provide tables of bounds on sizes of DNA codes with length from 1 to 9 and minimum distance from 1 to 9.