This paper describes an approach for fitting an immersed submanifold of a finite-dimensional Euclidean space to random samples. The reconstruction mapping from the ambient space to the desired submanifold is implemented as a composition of an encoder that maps each point to a tuple of (positive or negative) times and a decoder given by a composition of flows along finitely many vector fields starting from a fixed initial point. The encoder supplies the times for the flows. The encoder-decoder map is obtained by empirical risk minimization, and a high-probability bound is given on the excess risk relative to the minimum expected reconstruction error over a given class of encoder-decoder maps. The proposed approach makes fundamental use of Sussmann's orbit theorem, which guarantees that the image of the reconstruction map is indeed contained in an immersed submanifold.
翻译:本文描述了将一个有限维度的厄几里德空间的沉浸的亚磁层安装成随机样本的一种方法。 从环境空间到理想亚磁层的重建绘图是作为编码器的构成而实施的,该编码器每绘制一个点,显示一个(正或负)时间的图象,以及从固定初始点开始的有限多矢量场的流量构成所给出的解码器。编码器提供流动的时间。编码器解码器地图是通过实验风险最小化获得的,而高概率约束则显示相对于某一类别的编码器-解码图的预期最小重建错误而言的超风险。拟议方法基本利用了苏斯曼轨道的定理,这保证了重建地图的图像确实包含在浸入的子皮层中。