让我们来看看这个。大量的点一个问题。首先,太阳系。我们看不到任何碳氢化合物在太阳系内部(水星,火星)。这是因为在这一地区的太阳能系统,由太阳紫外线分解迅速破坏原始的碳氢化合物。这种效应弱得多。油井“补给”将在几十年发生在某种程度上,从内部迁移的石油。(通常只有一定比例的石油在地方恢复][1],与其他在孤立的口袋被水淹没。给它一个几十年,这些石油口袋会再迁移和联系,给予补充。我不知道你的评论*甲烷的来源方式太深来自化石。 No fossils involved.*. That's an unreferenced assertion. Helium is present in Natural Gas as a result of accumulation of alpha-decay particles from radioactive isotopes; we can see this from the massive enrichment of Helium-4 over [Helium-3][2]. It's not a paradox; geological structures that can trap methane will also trap helium. The current theory behind [petroleum geology][3] is that source rocks with a high organic content (often containing biological hydrocarbons from algae and leaf waxes) are buried in sedimentary basins; at temperatures around 100-150 degrees C this kerogen breaks down to form crude oils (this is verified in the lab). Oil then migrates out of this source rock; if it encounters a trapping geological structure, which need not be sedimentary, then it accumulates as an oil deposit. Gas is similar, with a wider range of source rocks. The physics of how this happens are [well known and established][4]. I would also note that we don't see hydrocarbons coming out of mantle-derived volcanoes such as at Hawaii. This is a major problem for any theory of primordial hydrocarbons. **Additional Points** First, it would be nice if you provided references rather than a link to a book to buy. 1. If hydrocarbons were primordial, then we would expect to find them mostly in areas where the mantle or mantle taps reach the surface - mid ocean ridges, and ocean island volcanoes. We don't. The major oil fields are located in continental extensional basin settings. 2. There is [plenty of evidence][5] for mantle outgassing - including all volatile species such as hydrocarbons - in the first few hundred million years. Furthermore, on geological timescales the mantle is still undergoing [vigorous convection][6] and can be considered liquid. 3. Is irrelevant. 4. This is simply wrong, if referring to pores that can offer any support against pressure. The crust becomes ductile at about 10-15km, and the mantle at 60+km, meaning that conventional porosity cannot exist. 5. See (1). For the Earth, outgassing was essentially completed billions of years ago, as we can see from isotopic evidence (and I suspect that the [moon-forming impact][7] didn't help). [1]: http://wiki.aapg.org/Reserves_estimation [2]: https://en.wikipedia.org/wiki/Helium-3 [3]: https://en.wikipedia.org/wiki/Petroleum_geology [4]: http://wiki.aapg.org/Plate_tectonics_and_basin_formation [5]: http://jgs.geoscienceworld.org/content/146/1/147 [6]: https://www.geophysik.uni-muenchen.de/research/geodynamics/mantle-convection [7]: https://en.wikipedia.org/wiki/Giant-impact_hypothesis