Based on the analysis of thermal contact metamorphic aureoles, granitoid interior structure, quartz axis fabric and strain characters in the different rock unites of yuanshishan granitoid and its wall rocks, the emplacement mechanism of yanshishan granitoid was studied. the magmatic explictite dynamic was advanced in light of regional stress and magma dynamic research. those conclusion was synthesized to ascertain the emplacement mechanism - granitic magma ascended in dikes with the minimum critical width of the magma ascending channels about 2. 213. 88m and located in the core of yindianshan dome with the passive style of dyke explictite ; the later unite is a kind of multiple emplacement mechanism with the character of active emplacement of ballooning
同時運用巖漿動力學原理從另一個角度探討其侵位驅動力。綜上指出：經分凝后的活動性巖漿在深部
側向擠壓和浮力的聯合驅動下，沿深大斷
裂以最小臨界寬度為2 . 213 . 88m的
裂隙脈動上侵，整體以巖墻擴展的方式被動定位於銀殿山穹窿的核部，但後期屋面前單元具有主動侵位的特點應為一種復合定位機制。
Through the search of bourn of intraclast congeries silica rock, its earth and west side all grow consortium robble
經對內碎屑堆積硅質巖的邊界研究發現，其東西兩
側均發育有同生斷
裂。
The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement
其後的繼承性活動在斷
裂帶內形成碎
裂程度最強達到碎
裂巖的碎
裂巖系列構造巖，變形帶兩
側發育兩組典型的共軛剪節理；第二次在晚白堊世?始新世，斷
裂在北東?南西向近水平擠壓作用下右行張扭性活動，斷
裂帶兩主斷
裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶，而斷
裂在巖體區也發育兩組典型的共軛剪節理，斷
裂內形成初碎
裂巖為主的構造巖；第三次是喜山期以西
側抬升、東
側下降的強烈升降為主的活動，在基巖中，主斷層兩
側圍巖出現微破
裂。
Hefei basin that is located on the southern fringe of the north china plate and by the side of tan - lu fault zone is a mesozoic cenozoic continental basin
合肥盆地為一中、新生代陸相盆地，位於華北板塊南緣、郯廬斷
裂帶西
側近旁
側。
These peaks correspond to side-chain cleavage of the ethyl and propyl groups respectively.
這些峰分別相當于乙基和丙基的
側鏈開
裂。
Delayed computed tomography scan with excretory phase revealed contrast medium extravasation from the left upj, and left renal pelvis rupture was diagnosed
但在延遲性的電腦斷層檢查后發現，顯影劑由左
側腎盂輸尿管接合處滲出，所以診斷為左
側腎盂破
裂。
Cluster analysis based on its pcr - rflp suggested that seven groups were distinguishable for pleurotus on 93 % similairity coefficient, i. e. p. oslrealus complex ( including p. ostreatus, p. florida, p. sapidus, p. corticalus, p. cornucopias, p. columbinus, p. spodoleucus, p. ferulae, p. nebrodensis and p. sp. ), p. eryngii, p. pulmonarius - p
Itspcr一rflp聚類分析結果表明， 52個
側耳菌株在93 %的相似系數水平可分為七類，第一類包括糙皮
側耳、佛羅以達
側耳、美味
側耳、
裂皮
側耳、黃白
側耳、哥倫比亞
側耳、灰自
側耳、阿魏蘑、白阿魏蘑;第二類為刺芹
側耳;第三類包括月
Cluster analysis based on rapd showed that at 76 % similarity level, all tested isolated could be clusted into nine groups, i. e. 1 p. ostreatus and p. florida, ii p. ostreatm p. sapidus, p. spodoleucus and p. eryngii, iii p. colnmbinus, p. corlicalus, p. cornucopiae, p. nebrodensis and p. ferulae ; iv p. pulmonarius and p. sajor - caju, v three isolates with indefinite species, vi p. luber - regium, vii p. cilrinopileatus, viii p. djamor and p. salmoneoslramincus, ix p. abalonus and p. cysliodism. 4. a single uniform product 1. 46kb in size resulted from pcr amplification of the 5 " half of the 28s rrna gene for all isolates of pleurolus and the other three genera
隨機擴增多態性dna的聚類分析表明，在76相似水平下，可將供試的
側耳菌株聚成九大類，第一大類包括糙皮
側耳、佛羅里達
側耳；第二大類包括美味
側耳、灰白
側耳、剌芹
側耳；第三大類包括哥倫比亞
側耳、
裂皮
側耳、黃白
側耳、阿魏蘑、白阿魏蘑；第四大類包括肺形
側耳和鳳尾菇；第五大類為3株未定名的
側耳；第六大類僅有具核
側耳；第七大類為金頂
側耳；第八大類包括紅平菇和桃紅
側耳；第九大類包括鮑魚菇和囊蓋
側耳。
The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference, the resistivity of the hanging wall is low and partially high, while that of the foot wall is high, and the faults are high - obliquity faults
沂水湯頭斷
裂、劉家莊斷
裂的二維電阻率反演結果表明，斷
裂帶兩
側的電性結構呈現出整體性的差異，正斷層的上盤為低阻區和局部高、低阻擾動區；而斷層下盤多為均勻的高阻區；斷層為高角度斷層。
The light bulb imploded
這燈泡是向內
側爆
裂的
In rift valleynarrowest place during, the natural megalith spans together, thenatural moat changes the thoroughfare ancient, the rift valley twosides cliffs 峙 立, wooden towering, the wild flower is brilliant, sight fluttering flags
在
裂谷最窄處，一塊天然巨石橫亙其間，天塹變通途，
裂谷兩
側懸崖峙立、古木參天、山花爛漫，風光旖旎。
The reasons and preventive measures of cracking in side - wall and top - plate of a multistory residential building
某高層住宅樓地下室
側墻與頂板
裂縫原因及防治
It is most efficient in clearing the peptide bonds on the c-terminal side of such amino acids tyrosine.
它對
裂開諸如酪氨酸這類氨基酸的羧基末端的
側肽鏈最為有效。
Sori borne along the longitudinal veins and protected by the reflexed edges of the ultimate segments of pinnules
孢子囊沿能育葉
裂片的縱脈兩
側著生，並為
裂片反卷的邊緣所覆蓋。
The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks
摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索
裂谷帶為沉積、沉降中心向南北兩
側展開的古地理格局：中晚侏羅世時期，
裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；
裂谷帶兩
側由濱淺海相碎屑巖和碳酸鹽巖組成。
Microsurgical treatment via small bone flap craniotomy through lateral fissure approach for hypertensive basal ganglia hemorrhage during ultra - early period
超早期小骨窗外
側裂入路顯微手術治療高血壓性基底節腦出血
In this slice, the lesion extends from near the occipital pole to the sylvian fissure, conforming to the territory of the posterior branch of the middle cerebral artery
在這一層，損害區從靠近枕骨粗隆延伸至至大腦外
側裂，與大腦中動脈后支支配的范圍相吻合。
According to baihetan hydroelectric power station dam shoulders load, side glide planes are fixed on both banks, which is controlled by base cracks on the left bank and by fault f18 and base cracks. and engineering geological characters of side glide planes
結合壩肩抗力體荷載特點，確定了壩肩抗力體側裂邊界，左岸主要由基體裂隙控制，右岸由斷層f18和基體裂隙共同控制，並研究了側裂邊界的工程地質性狀。
