mounds

mounds的基本解释

-

[变形] mound的第三人称单数

n.

土墩, 堤, 小山

vt.

筑堤, 用土堆防卫

vi.

积成堆

与mounds相关的网络例句 [注：此内容来源于网络，仅供参考]

The Carboniferous is a key period of the Phanerozoic reef evolution. There are mainly six common types of the Carboniferous organic reefs:(1) phylloid algal mounds,(2) stromatolic mounds,(3) coral reefs,(4) Waulsortian mud-mounds,(5) Chaetetes mounds,(6) microbial-algal mounds.

石炭纪是生物礁地史演化过程中一个非常关键的时期，发育的生物礁类型有：叶状藻礁丘；(2)叠层石礁丘；(3)珊瑚礁；(4)Waulsortian灰泥丘；(5)Chaetetes礁丘；(6)钙质微生物－藻礁丘。

Reefs, reef-mounds and lime mud mounds are all carbonate buildups, and the reefs and banks are important targets for petroleum exploration The reefs, banks and mounds should be divided from each other not only in theory, but also in exploration practice, because of so many differences in sedimentary compositions, fabrics, environments, distribution in time and space, and the characteristics of petroleum geology If the original reef or bank itself was fine reservoir rocks, then it would become a better reservoir after the reservoirconstructive diagenesis The formation of a high quality carbonate reservoir is controlled by two factors: the sedimentary microfacies and the reservoirconstructive diagenesis The first is the basis for the formation of a high quality reservoir, and with the high energy reefbank facies as the best; the latter includes the cataclasis, the dolomitization and the karstification The dolomitization and karstification are the best for the formation of a high quality reservoir The karstification has the widest distribution, profoundest effect, and plays a vital role in the high quality reservoir forming The karst types are quite rich in the limestone reef or bank reservoir, including synsedimentary karst, penesedimentary karst, supergene karst and hydrothermal karst, and so does the dolomitization reef or bank reservoir The formation mechanism of synsedimentary karst and penesedimentary karst is related to the short time exposing and leaching of the cyclical highfrequency shallowupward sequence when the reefs or banks are forming The supergene karst is controlled by the exposing and leaching of tertiary cyclic sequence type I interface after the reefs or banks forming Thus, there developed a great deal of secondary corrosion pores, corrosion fractures and huge caves besides some original pores remained in the reef and bank reservoir Scarcely there are any original effective pores in reefmounds and lime mud mounds, especially in senkes among mounds, but secondary pores could be formed by karstification, and there would likely develop source rocks with high organic abundance

礁、礁丘、丘同属碳酸盐建隆，礁、滩是重要勘探目的层。但各自在沉积组分、组构、环境和时空分布，以及油气地质条件上迥然不同，因而无论从理论还是勘探实践上，都有必要将其各成体系划分开来。礁滩自身为好储集岩，当建设性成岩作用叠加后可形成好的储层。碳酸盐岩优质储层形成，主要受沉积微相与建设性成岩作用两大因素控制。前者是基础，并以高能的礁滩相带为最好；后者主要包括破裂、白云石化和溶蚀三大类，并以白云石化或溶蚀为最优，其中的溶蚀分布最广泛、影响最深刻而对优质储层形成起决定性作用。礁滩储层中的古岩溶类型最为丰富多彩，包括同生期、准同生期、表生期和埋藏期热流体岩溶的所有类型，白云岩化礁滩体也不例外。其中，同生准同生期岩溶的形成机制与礁滩沉积时高频层序旋回向上变浅序列的短暂暴露淋溶有关，表生期岩溶则受控于礁滩沉积后三级层序旋回Ⅰ型界面的暴露淋溶。由此，导致礁滩储层中除了可以也是唯一保存原生孔隙外，还发育了次生溶蚀孔洞缝和大型溶洞。礁丘、灰泥丘尤其是丘间洼地中发育高有机质丰度烃源岩；它们自身没有有效的原生孔隙，但岩溶作用可以形成次生孔隙。

Green : In some ways, it draws off the original intentions for Midship, as a symmetric map built for CTF, with lines of sight that allow a defender to participate in the capture of an enemy flag without abandoning his post. Combat on the upper surface of the map has a flavor similar to Burial Mounds, though—or at least, the more cover rich areas of Burial Mounds.

A：某种意义上来说，设计隔离区的意图跟前作的船舰中央很接近——为夺旗模式设置的对称地形，互相可见的多个点让防守方找人方便而用不着到处转悠；地表高区的战斗更像前作的坟冢，至少很像坟冢的多掩体开阔地带。

与mounds相关的网络解释 [注：此内容来源于网络，仅供参考]

Shambling Mounds：(樹怪)

?Wickermen (柳樹妖) | ?Shambling Mounds (樹怪) | ?Coeurls (幻形獸)

Mounds：蒙兹

蒙杜 Moundou | 蒙兹 Mounds | 蒙艾利夫 Mount Ayliff

riprap mounds：乱石堆堤

rippling 齿面点蚀 | riprap mounds 乱石堆堤 | riprap 石堆堤

Boundary Mounds：分界丘陵

星门山Mensabaism | 分界丘陵Boundary Mounds | 焦骨平原Burntskull Wold

The Yi-min Mounds：義民塚

5 the colour of the rain 雨的顏色 | 6 the yi-min mounds 义民塚 | 7 tzu-tien station 莎呦娜啦竹田