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碎屑

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Shards:These are tiny fragments of castoff crystal imprinted with minisculebits of psionic power.

碎晶:这些都是丢弃的水晶碎片,其中留有细微的灵能碎屑

Middlings, warm water, apple parings , meat gravy, carrot scrapings, meat scraps, stale hominy, and the wrapper off a package of cheese.

麦麸,热水,苹果的碎屑,肉汁,胡罗卜皮,碎肉,不新鲜的玉米粥,以及干奶酪包装纸。

Sub-volcanic rocks include andesitic porphyrite, rhylitic porphyry, cryptoexplosive breccia as well as autobreccia etc.(2) Volcanic lithofacies——through the observation of cores, identification of thin sections and interpretation of well logs and seismic data, there are 8 kinds of lithofacies for the volcanic rocks of Yingcheng Formation are identified: fallout facies, effusion facies, pyroclastic flow facies, base surges facies, lahar facies, eruption-sedimentary facies, subvolcanic facies and extrusion facies.(3) Three types of eruption——i. e. explosion, effusion and surge.(4) Two kinds of eruptive environments——Subaerial (e. g. volcano in Well Shangshen 3) and subaqueous .(5) Three remarkable volcanic apparatus in Shengping-Wangjiatun area——layered, micro-shield and cone volcanoes according to volcanic processes and lithofacies distribution.

次火山岩有安山玢岩、流纹斑岩、隐爆角砾岩及自碎角砾岩等;(2)火山岩相——通过岩芯观察、镜下鉴定、测井与地震资料解释,营城组火山岩中发育8种岩相类型,即爆发空落相、溢流相、火山碎屑流、基底涌流相、喷发沉积相、火山泥石流相、侵出相和次火山相等;(3)火山喷发的形式——有爆发、溢流和涌流三种;(4)火山喷发环境——有陆上(如尚深3井火山)和水下两种;(5)火山机构类型——根据火山作用特点和岩相分布特征,在升平—汪家屯地区识别出三类截然不同的火山机构,即层火山、微型盾火山和渣锥火山。

The inflammation reaction hyperplactic stage and lymphatic nodular stage are of nonspecific morphological changes and should be diagnosed with the help of positive tuberculin test and obvious increase of adenosine deaninase ; tuberculous nodular stage has a great number of epithelioid cells,and Langhans cells, caseous necrosis stage is characterized by a great deal of necrotic tissue and debris,a small number of fragmented epithelioid cells, and mainly by antiacid bacteria fibrinous hyperplastic stage is featured by a few fibrous tissue, cells and mucous oweing to hardness to get puncture, which neans tuberculous restoration,and scar formation.

炎性增殖反应期非特异性形态学变化,需要结合结核抗体阳性和腺苷酸脱氨酶明显增高有助于诊断,结核结节期主要可有较多类上皮样细胞及郎罕氏细胞;而干酪样脓样坏死主要见大量坏死组织及碎屑、少数残碎不全类上皮样细胞,此期主要能查到抗酸菌为特征;纤维增殖期,抽出物难取,仅见少数纤维组织、纤维细胞和黏液间质为其特征,提示结核恢复、瘢痕形成所致。

The inflammation reaction hyperplactic stage and lymphatic nodular stage are of nonspecific morphological changes and should be diagnosed with the help of positive tuberculin test and obvious increase of adenosine deaninase ; tuberculous nodular stage has a great number of epithelioid cells,and Langhans cells,caseous necrosis stage is characterized by a great deal of necrotic tissue and debris,a small number of fragmented epithelioid cells,and mainly by antiacid bacteria fibrinous hyperplastic stage is featured by a few fibrous tissue,cells and mucous oweing to hardness to get puncture,which neans tuberculous restoration,and scar formation.

炎性增殖反应期非特异性形态学变化,需要结合结核抗体阳性和腺苷酸脱氨酶明显增高有助于诊断,结核结节期主要可有较类上皮样细胞及郎罕氏细胞;而干酪样脓样坏死主要见量坏死组织及碎屑、少残碎不全类上皮样细胞,此期主要能查到抗酸菌特点;纤维增殖期,抽出物难取,仅见少数纤维组织、纤维细胞和黏液间质为其特征,提示结核恢复、瘢痕形成所致。

The inflammation reaction hyperplactic stage and lymphatic nodular stage are of nonspecific morphological changes and should be diagnosed with the help of positive tuberculin test and obvious increase of adenosine deaninase ; tuberculous nodular stage has a great number of epithelioid cells,and Langhans cells, caseous necrosis stage is characterized by a great deal of necrotic tissue and debris,a small number of fragmented epithelioid cells, and mainly by antiacid bacteria fibrinous hyperplastic stage is featured by a few fibrous tissue, cells and mucous oweing to hardness to get puncture, which neans tuberculous restoration,and scar formation.

炎性增殖反应期非特异性形态学变化,需要结合结核抗体阳性和腺苷酸脱氨酶明显增高有助于诊断,结核结节期主要可有较多类上皮样细胞及郎罕氏细胞;而干酪样脓样坏死主要见大量坏死组织及碎屑、少数残碎不全类上皮样细胞,此期主要能查到抗酸菌为特点;纤维增殖期,抽出物难取,仅见少数纤维组织、纤维细胞和黏液间质为其特征,提示结核恢复、瘢痕形成所致。

The inflammation reaction hyperplactic stage and lymphatic nodular stage are of nonspecific morphological changes and should be diagnosed with the help of positive tuberculin test and obvious increase of adenosine deaninase ; tuberculous nodular stage has a great number of epithelioid cells,and Langhans cells, caseous necrosis stage is characterized by a great deal of necrotic tissue and debris,a small number of fragmented epithelioid cells, and mainly by antiacid bacteria fibrinous hyperplastic stage is featured by a few fibrous tissue, cells and mucous oweing to hardness to get puncture, neans tuberculous restoration,and scar formation.

结核初期-炎性增殖期60例,占5.5%;结核早期-淋巴结节期130例,占11.9%;结核中期-结核性结节期有590例,占54.1%;结核晚期-干酪样脓样坏死期有280例,占25.7%;结核恢复期-纤维素增殖期30例,占2.8%。炎性增殖反应期非特异性形态学变化,需要结合结核抗体阳性和腺苷酸脱氨酶明显增高有助于诊断,结核结节期主要可有较多类上皮样细胞及郎罕氏细胞;而干酪样脓样坏死主要见大量坏死组织及碎屑、少数残碎不全类上皮样细胞,此期主要能查到抗酸菌为特点;纤维增殖期,抽出物难取,仅见少数纤维组织、纤维细胞和黏液间质为其特征,提示结核恢复、瘢痕形成所致。

On the basis of the analyses of peripheral ancient land, light and heavy mineral associations, the cathodoluminescence color of quartzes, the typomorphic characteristics of various debris and directions of palaeoflow, it is considered that detrital material of terrigenous origin of the Upper Palaeozoic in this area come from north provenance, Yimeng uplift in the northern part of Ordos Basin.

根据盆地周缘古陆、轻、重矿物组合、石英阴极发光颜色、各种岩屑的类型特征及古水流方向等特征的分析,认为研究区上古生界陆源碎屑物质来自北部物源区,即盆地北部的伊盟隆起地区。

The Middle Devonian Beitashan Formation consists of a series of intermediate-basic volcanic rocks intercalated with more than 100 m thick picritic layer at the bottom, whereas the Middle Devonian Yundukala Fm. is composed of a series of shallow-sea fine-clastic rocks interbedded intermediate rocks and intermediate-basic rocks. The Late Devonian Jiangzierkuduke Fm. includes pyroclastic rocks intercalated with intermediate-basic and intermediate-acid rocks, whereas the Late Carboniferous Batamayineishan Fm. consists chiefly of basalts and basaltic andesites intercalated with tuff, siltstone and carbonaceous shale.

其中中泥盆世北塔山组为一套中基性火山岩,并且底部含有厚度超过100m的苦橄岩;中泥盆世蕴都喀拉组为一套浅海相细碎屑沉积岩夹中性、中基性火山岩;晚泥盆世江孜尔库都克组为火山碎屑岩夹中基性和中酸性火山岩组合;而晚石炭世巴塔玛依内山组以玄武岩和玄武安山岩为主,夹凝灰岩、粉砂岩和炭质页岩。

Unlike igneous rocks which are formed from molten rock material, sedimentary rocks are made up of particles of previously existing rocks, including igneous, metamorphic and sedimentary rocks.

沉积岩不像火成那样是由熔融的岩石物质形成,沉积岩是由早先存在的浆岩,变质岩和沉积岩的矿物碎屑及岩石屑组成的

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