Prismatic and q-crystalline sites of higher level
Abstract
In this article, we define the m-prismatic site and the m-q-crystalline site, which are higher level analogs of the prismatic site and the q-crystalline site respectively. We prove a certain equivalence between the category of crystals on the m-prismatic site (resp. the m-q-crystalline site) and that on the prismatic site (resp. the q-crystalline site), which can be regarded as the prismatic (resp. the q-crystalline) analog of the Frobenius descent due to Berthelot and the Cartier transform due to Ogus-Vologodsky, Oyama and Xu. We also prove the equivalence between the category of crystals on the m-prismatic site and that on the (m-1)-q-crystalline site.
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