| 1. | Combination features of depositional sub - facies of debris - flowon the jiangjiagou valley , yunnan province
东川蒋家沟泥石流沉积亚相组合特征 |
| 2. | It was developed mostly deep lake facies on the south of basin and coastal - shallow lake facies on the north of basin
此时期盆地南缘主要发育半深湖亚相，盆地北缘则发育滨浅湖亚相。 |
| 3. | Differences among the subfacies or microfacies displayed in terms of petrology , texture , structure and so on
各亚相之间和各微相之间的差别主要体现在碎屑岩的岩性、结构、构造等方面。 |
| 4. | Traditionally , various subphase belts for irruptive rock body are studied and analyzed by mainly drilling well and coring
传统上对侵入岩体各亚相带的研究和判断，主要通过钻井取心来认识。 |
| 5. | Vocalnic activity characterizes extru - sive facies - spurt - deposit facies , which constitutes multi - rhythmic volcanic spurting
火山活动具有由喷发相(喷溢亚相) -喷发-沉积相的特点，构成了具多韵律性的火山喷发特征。 |
| 6. | Sand bar sub - facies of lagoon , front delta , sheet sandstone of offshore sea are the best sedimentary facies belts for the oil & gas accumulation
泻湖相堡坝亚相、三角洲相前缘亚相以及滨海相席状砂亚相是砂岩储层分布和发育的最有利相带。 |
| 7. | High heterogeneity of the reservoir quality of the chang - 2 oil - bearing beds reflected primarily in the facies , subfacies and microfacies , and the fluid unit of the microfacies as well
长2油层组储层物性表现出明显的非均质性，其非均质性表现在相、亚相以及微相内部的流体单元之间。 |
| 8. | The optimized condition is : urease concentration 8 mg l " 1 , ph value of subphase 5 . 5 , association time of ureaes with amphiphiles 2 h , the temperature of subphase 10 ? , sio2 / si substrate with hydrophobic surface
脲酶浓度8mgl ~ ( - 1 ) ，亚相ph值5 . 5 ，酶与表面单分子膜的缔合时间2h ，亚相的温度10 ，基片表面为憎水性。 |
| 9. | 3 . the film - forming property of ruhb and it ' s adsorphon with human serum albumin ( l ) it is concluded bom n - a isotherm curves on subphases with arerent ph values that the film - formin property of hihb am be better improved on alkaline subphases
（ 2 ）利用。 a等温曲线和。 t时间曲线研究了不同酸度的亚相上人血清白蛋白（ hsa ）吸附在hihb单分子膜上的情况。 |
| 10. | Being primarily controlled by northwest faults , cretaceous of jiyang depression contained several isolated basins , and lake levels of these isolated basins were instable , but on the whole , shore and shallow lake sub - facies is in the majority
北西向断层的活动对沉积起到主要的控制作用，在其控制下，白垩纪济阳坳陷为一相互分割的山间盆地，湖盆范围时大时小，湖水深度不断变化，总体湖水较浅，主要发育滨浅湖亚相。 |
