Super Climax [TOP]
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Super Climax [TOP]
Climax Form (クライマックスフォーム, Kuraimakkusu Fōmu) is Den-O's super form, gained when all Tarōs but Momotaros faded away and Ryotaro's desire not to lose them created the K-Taros cell that is attached to the Den-O Belt once the code 3-6-9-# is entered. Climax Form is basically a stronger version of Sword Form that incorporates the DenKamen of the other three primary Den-O forms onto various parts of the armor.
There are plenty of examples of this mechanic throughout the genre. For instance, the Street Fighter EX series and its follow-up Fighting EX Layer use move-canceling to chain multiple super moves together. Furthermore, the Marvel Vs. Capcom series has a mechanic that allows players to cancel one team member's super combo into a partner's super combo.
On the one hand, you'll notice that super cancels out of special moves require the fastest inputs since special moves have fewer animation frames. On the other hand, Climax canceling out of a more extended MAX Super Special move gives you a longer input window.
Speed is an essential requirement for move-canceling. After all, the point of a move-cancel is to cut an animation short. In turn, your input window is no longer than the current move's animation. When canceling from one Super Special move into a MAX or Climax move, that's a decent chunk of time. However, super canceling out of a special move requires some quick reflexes.
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[Convulsions over 1000 times] [Unstoppable super climax] [Sweaty raw fuck 2 consecutive ] [Extremely erotic ] This is gone! Is the word erotic for this gal! ! The harmony of convulsions and climax summons a wave of excitement and sparks! ! !
[Deca Hip Party] [Cream Pies & Blow Job 3 Consecutive Shots] [Hyper Convulsive Climax] [Amazing Erotic Butt God] [Infinity Fucking Tide] Let's start the deca hip party! ! From jerking and super convulsions Doero Kamijiri swaying blurun! !
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The high flux of magma associated with super eruptions is hypothesized to rebuild the deep crust, altering the source(s) of subsequent magmatism. Climax-type Mo deposits are commonly generated immediately after eruption of large ignimbrites within a volcanic field, and provide an opportunity to understand the evolution of magma sources following high flux events. The Questa caldera of the Latir volcanic field, NM exposes a 10 Ma long record of pre-, syn- and post-ignimbrite intrusive and extrusive rocks, and hosts the Questa Climax-type Mo deposit. New detailed geochronology and geochemistry from Questa (including extensive sampling of subsurface rocks in the mine) permit detailed reconstruction of the temporal evolution of magma sources through the waxing and waning stages of super eruption magmatism. Comparison of chemical and isotopic data waxing, ignimbrite, Mo-mineralizing and waning stage magmas reveals several patterns. Waxing and waning magmas (waxing: 29-25.7 Ma; waning: 24.5-19 Ma) have intermediate trace elements and radiogenic isotopes relative to other magmatism (87Sr/86Sri=0.7050 to 0.7070, ɛNd=-5.2 to -7.2). Ignimbrite magmatism (25.5 Ma) is depleted in incompatible elements, enriched in MREE and HREE's and has more evolved radiogenic isotopes (87Sr/86Sri=0.7095, ɛNd=-8.0). Molybdenum mineralizing magmas (24.9-24.5 Ma), are enriched in incompatible elements, depleted in MREE and HREE's and have distinct radiogenic isotopes (87Sr/86Sri=0.7055 to 0.7075, ɛNd=-4.2 to -5.7). We suggest the lower crustal source of magmas changed during ignimbrite generation, and as a result, subsequent mineralizing magmas incorporated more juvenile, mafic components. This mantle influence is the metallogenesis for Climax-type deposits and indicates that deep crustal hybridization, rather than upper crustal differentiation, is pivotal in their generation. These results indicate that a lower crustal source of magmatism for a volcanic field is altered due to super eruptions. 153554b96e
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