海洋地壳是由(玄武岩)[1]和[2](辉长岩)和沉积材料。我们知道,由于钻粉和化石(蛇)[3]:> [!(蛇绿岩截面)[4]][4]>来源:[林克之。金泽][5][6](墨西哥湾)也不例外,(沉积物)[7](不像你提到沉积岩问题),作为本文说:>“大多数沉积物源于相邻的土地,主要通过河流运输。直接沉淀碳酸钙和矿物质蒸发主要发生在佛罗里达和尤卡坦平台和一些沿海泻湖。深海环境往往是由陆源和生物沉积物泥。”(Davids Jr, R.A.,2017) [1][8] [Caribbean Sea][9] is neither an exception, as remarcks Encyclopedia Britannica in this article: >"The ancient sediments overlying the seafloor of the Caribbean, as well as of the Gulf of Mexico, are about a half mile (about one kilometre) in thickness, with the upper strata representing sediments from the Mesozoic and Cenozoic eras (from about 252 million years ago to the present) and the lower strata presumably representing sediments of the Paleozoic and Mesozoic eras (from about 541 to 66 million years ago)" (Menzies,R.J. et al, 2019) [2][10] This article says there is one kilometer of sedimentary materials, enough to [diagenesis][11] to take place and so, there are [sedimentary rocks][12] under the unconsolided sediments. -------- 1) [**Davis R.A. (2017)** *"Sediments of the Gulf of Mexico."* In: Ward C. (eds) **Habitats and Biota of the Gulf of Mexico: Before the Deepwater Horizon Oil Spill**. Springer, New York, NY][8] 2) [**Menzies, R.J., Ogden, J.C. (2019)** *"Caribbean Sea."* In: **Encyclopedia Britannica**.][10] [1]: https://en.wikipedia.org/wiki/Basalt [2]: https://en.wikipedia.org/wiki/Gabbro [3]: https://en.wikipedia.org/wiki/Ophiolite [4]: https://i.stack.imgur.com/UL4RD.gif [5]: http://earth.s.kanazawa-u.ac.jp/ishiwata/ophiol_e.htm [6]: https://en.wikipedia.org/wiki/Gulf_of_Mexico [7]: https://en.wikipedia.org/wiki/Sediment [8]: https://link.springer.com/chapter/10.1007/978-1-4939-3447-8_3#citeas [9]: https://en.wikipedia.org/wiki/Caribbean_Sea [10]: https://www.britannica.com/place/Caribbean-Sea [11]: https://en.wikipedia.org/wiki/Diagenesis [12]: https://en.wikipedia.org/wiki/Sedimentary_rock