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Armed with this information and further analyses, Rumble, lead author Bekker, and colleagues propose the following scenario today in Science . Early in Earth's history, volcanic eruptions spewed massive amounts of sulfur dioxide into the atmosphere, where UV sunlight broke down the gas and created the odd sulfur isotope ratios. The sulfur descended with the rain and accumulated into sedimentary beds on the sea floor. Once there, superheated water from geothermal vents at various locations on the sea floor cooked the sulfur into sulfide. Finally, nickel-bearing magma welled up from Earth's mantle, combining with the sulfide to form nickel sulfide and encasing the compound inside volcanic rock called komatiite.

凭借这份资料和进一步的分析,朗布尔、研究论文的第一作者贝克及同事们今天在《科学》杂志上提出了如下的推测:在地球早期的历史上,火山爆发将大量的二氧化硫气体喷射到空中,太阳的紫外线将其分解,产生了奇特的硫同位素比值,这种硫随雨降下,积存于海底沉积层中;一旦到达海底,海底各处的地热出口所产生的温度过高的水把硫加热成硫化物;最终含有镍的岩浆从地幔中涌出,跟硫化物结合形成硫化镍,并将硫化镍包裹在一种叫做"科马提岩"的火山岩中。

Combined with subsea tunnel engineering at eastern route way in Xiamen,the minimum rock covering thickness of subsea tunnel,water pressure design values,section optimization of lining structure and waterproof and drainage project,construction measures throughout bad subsea geology section,such as fault,solution groove,necessity of service tunnel setting were analyzed.

结合厦门东通道海底隧道工程,对海底隧道最小岩石覆盖层厚度、水压力设计值的确定,衬砌结构断面优化与防排水方案,穿越海底不良地质段的施工措施及服务隧道设置的必要性问题进行了分析。

Considering the properties of hydrate formation, the designing principle of drilling fluid was provided. Based on this, a new polyalcohol drilling fluid for oceanic hydrate formations was formulated. The performance of this drilling fluid was evaluated by shale hydration inhibiting test, low-temperature rheological property test, and gas hydrate formation inhibiting experiment.

针对海底天然气水合物地层及其钻井的特性,给出了钻进海底天然气水合物地层时钻井液体系的设计原则,根据此原则在充分考虑现有常用聚合醇钻井液体系特点的基础上,设计了一种适合海底天然气水合物地层钻井的新型聚合醇钻井液,并对其页岩水化抑制性、低温流变性和水合物生成抑制性进行了评价。

Based on scene X fluorescence analysis ray fluorescence , X of sea floor , that principle develop survey system can go on normal position survey to the sediment in sea floor, can carry on non- destructive analysing to the sediment of sea floor that is gathered fast on the ship too, mineral products reconnoitre or environment investigate in time submitting necessary information for marine.

基于现场X荧光的分析原理研制的海底X射线荧光探测系统可在海底对沉积物进行原位测定,也可以在船上对采集的海底沉积物进行非破坏性的快速分析,为海洋矿产勘察或环境调查及时提供必要的信息。

The acceleration and sound pressure on the surface of seafloor are obtained.

建立了点声源作用下海底地震波的时域数值计算模型,利用该模型,对二维半无限空间简单海洋模型的低频点声源海底地震波问题进行了数值模拟,得到了海底表面处的加速度和声压值。

Japanese scholars of Japan and South Korea proposed a three-tunnel routes, two from Kyushu in Japan through the Tsushima Strait Karatsu Geoje Island, South Korea, one from Japan to Pusan, South Korea Karatsu, submarine length between 128-148 km, than the distance between China and South Korea are also much closer, but still is the famous Anglo-French tunnel four times.

日本学者提出的日韩海底隧道路线有3条,两条从日本九州的唐津市经对马海峡到韩国巨济岛,一条从日本唐津到韩国釜山,海底长度在128公里至148公里之间,比中韩之间的距离也近许多,但仍是著名的英法海底隧道的4倍左右。

Unique in Mauritius, this underwater submarine invites you to live a rare experience: go down to a depth of 35 to 40 metres amidst a mass of coral from where you can contemplate numerous multicoloured fish species, wreckages, anchors and other neglected treasures at the bottom of the sea..

毛里求斯独一无二的体验,乘坐潜水艇将会给您留下珍贵的回忆:让您潜入到35到40米深的水下,置身于珊瑚丛中,观赏五光十色的海底鱼类,看看沉没于海底多年的古船残骸、旧锚,或者探索其它什么早已被人忽略的海底传奇。。。。。。

Seismic energy is disturbed and attenuated seriously under the bad geological conditions for seismic exploration in southern Huanghai basin, and therefore the Meso-Paleozoic wave group of marine reflection seismic cannot be recognized and the seismogram does not meet the requirement for evaluation of pre-Tertiary oil/gas resources in southern Huanghai basin. In May 2006, marine magnetotelluric sounding experiment was carried out and reliable data were acquired.

针对南黄海盆地深层地震地质条件差,地震波受屏蔽,能量严重衰减,在海洋反射地震资料中很难识别反映中-古生界的反射地震波组,不能满足南黄海盆地前第三系油气资源前景评价的需要等问题,于2006年5月,开展了南黄海海域海底大地电磁测深试验,在盆地内五莲斜坡和胶州凹陷区布设了3个海底大地电磁测深点,取得了可靠的海底观测数据。

An algorithm for decomposition of multi wave and multi component data into upgoing and downgoing P wave and S wave was derived in frequency wave number domain in this paper. The reflection coefficient versus incident angle was calculated, which can provide foundational data for the AVO inversion of elastic parameters and prediction of fluid factor.

在频率波数域中采用解析法,解出多层条件下海底实测的多分量地震数据分解成上行和下行P波和S波的算法,导出海底各层地震反射系数随入射角变化的递推计算公式,为海底多波多分量AVO弹性参数的反演及流体因子预测提供基础数据。

We analyze the distribution of temperature and heat flow of the sea floor sediment in the area of East China Sea slope and West basin area of the Okinawa Trough.

利用实测的海底温度和海底热流资料对东海陆坡和冲绳海槽中轴以西的槽底地区的海底温度场和热流场进行了分析。

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