WIC-Venus Ejection Hypothesis (VEH): A Stratified Disruption Model for Early Solar System Evolution and Lunar Origin — Self-Contained Deduction Volume V3.6 & Academic Main Text V5.5.3 (Two-File Preprint) ZH(对照,不填表单,仅留档与对外中文说明用): WIC-金星分层剥离假说(VEH):太阳系早期演化与月球起源的分层剥离模型——全自足推演册合卷V3.6与学术正文V5.5.3(双文件预印本)

The origin of the Moon and the early evolution of the inner solar system remain central unresolved problems in planetary science. This deposit presents the Venus Ejection Hypothesis (VEH): in the early Solar System, primordial Venus was a differentiated, rapidly rotating (P in [3,12] h), globally molten body in an assist-disruption state; driven by periodic Jupiter-Saturn cross-configuration tidal modulation and Venus-Earth orbital phase windows, it underwent the B3 stratified material redistribution — appearing macroscopically as stratified pulsed transport spanning >= 200 Myr: each pulse is a short-duration (tens of days) parcel eruption that first feeds a circum-Venus debris disk, with final escape completed by subsequent multi-period resonant pumping. The four-layer structure of primordial Venus (atmosphere, volatile ocean, magma ocean, solid core) was exported batch-wise: part of the silicate material accumulated gradually within Earth's Hill sphere to form the Moon, part fell onto Earth, and the rest was diverted into the asteroid belt, outer-planet irregular-satellite systems and the Oort-cloud comet reservoir. Upon completion, Venus reaches a retrograde-spin final state. Six falsifiable predictions with explicit failure conditions are presented (deep-lunar oxygen-isotope offset; glass-dominated C-type asteroids; comet D/H sub-populations after subtracting the local background; deep-Venus layering; early redox pulses; isotopic-fingerprint clustering of pulse batches pointing to a Venus source). Trigger mechanisms and allocation fractions are deferred to SPH/N-body verdict protocols. This is a working alternative hypothesis, not an experimentally confirmed theory. ZH: 月球起源与内太阳系早期演化是行星科学的核心难题。本存档提出金星分层剥离假说(VEH):太阳系早期,原始金星为分层、快速自转(周期3–12小时)、全域岩浆海的辅助剥离态行星;受木星-土星十字构型长周期潮汐调制与金-地轨道相位窗口驱动,发生B3分层物质再分配——宏观表现为横跨≥200 Myr的分层脉冲式物质输运:单脉冲为短时(数十天级)团块喷发,物质先进入环金星碎屑盘,逃逸由后续多周期共振泵浦逐步完成。原始金星四层结构(大气/挥发物海洋/岩浆海/固态核)分批向外输运:部分硅酸盐在地球希尔球内渐进堆积形成月球,部分坠落地球,其余分流至小行星带、外太阳系卫星系统与奥尔特云彗星库。演化完成后金星达逆向自旋终态。本文给出六项带明确失效条件的可证伪预言(月球深部氧同位素偏移、C型小行星玻璃质主导、彗星D/H扣除本地背景后的子分布、金星深部分层、早期氧化还原脉冲、脉冲批次同位素指纹聚类指向金星源);触发机制与分配份额交由SPH/N-体判决协议裁决。本文为工作假说,非已证实理论。