冷泉碳酸盐

这些微生物通过生命代谢过程，使渗漏系统中的CH4被氧化转变为CO2，同时孔隙水中的SO4~（2-）还原成H2S，与Ca和Fe离子结合沉淀冷泉碳酸盐岩。

These bacteria collaborate to oxidize venting methane to CO2 and reduce seawater sulfate to H2S by their metabolism in the seeping system . The abundance of COi and HaS , causes the seep carbonate to be deposited .

海底甲烷缺氧氧化与冷泉碳酸盐岩沉淀动力学研究进展

Anaerobic oxidation of methane and seep carbonate precipitation kinetics at seafloor

墨西哥湾陆坡区冷泉碳酸盐岩的烷烃分布特征

Alkane distributions of seep-carbonates from the slopes of Gulf of Mexico

海底天然气渗漏系统微生物作用及冷泉碳酸盐岩的特征

Characteristics of Cold Seep Carbonates and Microbial Processes in Gas Seep System

南海北部陆坡九龙甲烷礁冷泉碳酸盐岩沉积岩石学特征

Petrographic characteristics of authigenic carbonates from Jiulong methane reef of northern South China Sea

墨西哥湾布什山冷泉碳酸盐岩沉积岩石学及地球化学

Geology and geochemistry of seep carbonates from Bush hill of the Gulf of Mexico

南海北部大陆坡冷泉碳酸盐结核的发现：天然气水合物新证据

Discovery of seep authigenic carbonate nodules on northern continental slope of South China Sea : New evidence of gas hydrate

中碳镍铬钼钢中夹杂物和韧窝断口形貌关系的初步观察南海北部冷泉碳酸盐岩矿物微形貌及其意义探讨

ON THE RELATION BETWEEN INCLUSIONS AND MORPHOLOGY OF DIMPLE FRACTURES IN CERTAIN STEELS Minerals ' Micro-Shape and Its Significance of Seep Carbonates in the North of the South China Sea

通过对2002年广州海洋地质调查局在南海北部海域拖网采集的碳酸盐岩样品进行岩石、矿物、微量元素和同位素特征的研究，证实在南海水合物远景区发育有冷泉碳酸盐岩。

The carbonate samples described in this paper were collected by Guangzhou Marine Geological Survey in April 2002 from the northern continental slope of the South China Sea using the tow-net samples .

海底天然气渗漏系统甲烷氧化细菌特征及其产物-冷泉碳酸盐岩的微观分析表明，冷泉碳酸盐岩保存了大量的以纳米为主的细菌化石。

The microanalyses show that bacteria fossils mostly in nanometer scale were preserved greatly in their byproduct-seep carbonates collected in the gas seeping system in GC 238 , the offshore Louisiana Gulf of Mexico .

渗漏晚期，天然气渗漏速度很慢（q<0.55kg/m2a），在海底附近没有水合物沉淀，主要以冷泉碳酸盐岩发育为主，水合物产于海底之下一定深度的沉积层中。

The venting rates are slow ( gas flux q < 0.55 kg / m ~ - a ) in the later stage , hydrate crystallization will not reach the sea floor , seep carbonate will be occurred on the seafloor .

海底天然气渗漏不仅影响海底沉积物的物理性质，而且还极大地改变海底地形地貌，它能在海底形成麻坑、泥火山、冷泉碳酸盐岩以及化学自养生物群落等现象。

Marine gas seepage not only influences the physical properties of the seafloor sediments , but also significantly alters the geomorphology of the seafloor , such as the occurrence of pockmarks , mud volcanoes , authigenic carbonate and cold seep communities on seafloor .

冷泉及冷泉碳酸盐岩是当今科学界研究的前沿之一。

Cold seep and cold seep carbonates are the frontiers in the modern science .