| 1. | Restudies on permian reefs in eastern sichuan , china
川东二叠纪生物礁的再认识 |
| 2. | Ordovicion reef in lunan - bachu area and their reservoir characteristics
巴楚地区奥陶系生物礁储层特征 |
| 3. | Stratigraphic sequence of the early - middle permian reef in western east kunlun mountains
中二叠世生物礁相地层层序 |
| 4. | Abundant and various reefs with conspicuous physical properties and high reserves have widely developed in western qaidam basin
摘要柴西地区发育了储集物性极好、分布较为广泛、储量较高的生物礁储层。 |
| 5. | In studied areas , reefs of western areas grew bigger in dimensions than those of the eastern , and the strata in which caning reefs became upper
鄂西渝东区生物礁从西往东逐渐增大，发育层位逐渐抬升，与由东向西的海侵有关。 |
| 6. | The reefs widely developed from sinian to neogene in china , with main reef - forming stages in devonian , permian and neogene , respectively
摘要中国生物礁从震旦纪至新近纪均有发育，分布范围广，并有泥盆纪、二叠纪和新近纪3个主要造礁期。 |
| 7. | The development of reefs was controlled by the tectonic setting , sea - level movement , paleogeographic environment and evolution of reef - forming organisms
生物礁的发育受构造作用、海平面变化及古地理环境控制，同时也受造礁生物兴衰演化的控制。 |
| 8. | This paper reviews the log responses of various types of bioherms using core and well log data , and proposes the features of logs suitable for these biohermal reservoirs
但湖相生物礁在柴西地区分布不均，变化很大，难以用传统的方法进行勘探和开发。 |
| 9. | Reefs or bioherms are an impotant type of carbonate deposits . they are consist of numerous and all kinds of organisms , or resulted from biological action
生物礁是碳酸盐沉积中的一种重要类型，这是由大量的、各种各样的生物堆积而成，或是生物作用的产物。 |
| 10. | And the reefs can be divided into three types : reefs developed in the margin of platform , mud mound in the low slope and patch reefs within the platform
黄泥塘一带属红椿湾边缘下斜坡的泥丘礁或生物灰泥丘。建7井区、石宝寨、老龙洞等生物礁则属于台内点礁。 |
