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首页> 外文期刊>Geophysical Research Letters >Tectonic Uplift Destabilizes Subsea Gas Hydrate: A Model Example From Hikurangi Margin, New Zealand
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Tectonic Uplift Destabilizes Subsea Gas Hydrate: A Model Example From Hikurangi Margin, New Zealand

机译:构造隆起使海底天然气水合物:来自新西兰Hikurangi边缘的模型例子

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摘要

Rising ocean temperatures and falling sea level are commonly cited as mechanisms of marine gas hydrate destabilization. More recently, uplift-both isostatic and tectonic-has been invoked. However, the effect of tectonic shortening and uplift on gas hydrate stability zone extent has not been validated via integrated computational modeling. Here, modeling along the Hikurangi margin of New Zealand illustrates the mechanism of tectonic uplift as a driver of gas hydrate destabilization. We simulate how tectonic uplift and shortening affect the presence and decrease the extent of a gas hydrate stability zone. We suggest that resultant gas hydrate destabilization in the marine realm may impact the global carbon cycle and oceanic chemistry over geologic time.
机译:海洋温度和海平面上升通常被引用为海洋气体水合物不稳定的机制。 最近,已经调用了隆起 - 异位和构造。 然而,通过集成计算建模尚未验证构造缩短和隆起对气体水合物稳定区的影响。 在这里,沿着新西兰的Hikurangi边缘建模说明了构造隆起的机制作为天然气水合物不稳定的驾驶员。 我们模拟了构造隆起和缩短如何影响存在和降低气体水合物稳定区的程度。 我们建议在海洋境界中产生的天然气水合物不稳定可能影响全球碳循环和海洋化学在地质时间上。

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