The elemental geochemical anomaly of pore water in Marine sediments during the formation of gas hydrate is a significant indication for Marine gas hydrates in the deep sea floor.
Such contributing factor form all in the interest of Hua Lixi stage the Marine facies volcanic rock moulds, the formationMarine facies volcanic rock succeed mine set.
其成因类型均为华力西期海相火山岩型，形成海相火山岩成矿系列。
3
There are at least three reservoir cases in deepwater: Eocene terrestrial formation, low Oligocene transitional formation and Pliocene and above Marine deepwater fans.