Foreign SCI on the geochemistry of mineral deposits which is easy to publish

Scientific research has no actual content, and it is not easy to publish.

It depends on what you do, write a review and send "Ore Geology Review", if it is a relatively blank area in the world, you can also send "International Geology Review", the latter is less difficult than the former, in addition, it depends on how you work to make mineral deposits, what you have done, and you can send "Canadian Minerologist" and "America Minerologist" when you do minerals. A section of the characteristics of the deposit is called "economic geology", and you can also consider "mineralium deposita", but this is more difficult to occur, and you can consider "chemical geology" for applied geochemistry, the impact factor is relatively high, and the English requirements are not low; However, it is more refined and specialized, and you can also consider "geology" for a unique introduction, which requires concise language and proper use. There are many more, which can be found on the Internet. However, you can consider finding some English journals that are not in English-speaking countries, which are relatively simple, and there are some in Europe, look for them, and find them here, haha!

The review of geoscience journals is relatively long, and the review should be relatively fast in half a year, mainly depending on your article, which is consistent with the reviewer's interest, and it will be completed soon, and there is a bit of a discrepancy, so you have to wait.

C=C double bonds can be transitioned, and since the nucleus does not control the electron as well as the electron, the energy required for the transition is less than that of the electron. Therefore, the *transition value is larger, around 5000 100000, but only one c=c double bond transition occurs at 170 200nm, which is absorbed in vacuum ultraviolet and cannot be observed by a general spectrophotometer. For example, the transition of ethylene, max=185 nm (=10000), is not detectable in the near-ultraviolet region, and the absorption of the same transitions as c c and c n is less than 200 nm.

If there is a common yoke system formed by two or more double bonds (including triple bonds) in the molecule, the electrons are in the molecular orbital of the delocalized delocalization, and the energy difference between the highest energy level of the bonding orbital that occupies the electron and the lowest energy level of the antibond orbital that does not occupy the electron is reduced compared with the localized orbital, so that the energy required for the transition is reduced, and the absorption is displaced in the direction of the long wave. The extinction coefficient also increases, for example, two pairs of electrons in the 1,3-butadiene molecule fill the bonding orbitals of 1 and 2, and the antibonding orbitals of 3 and t4 are empty, and the transition from 2 to 3 occurs when the electrons absorb the required light energy.