关于PEL型Shimura变种的Hecke轨道猜想

IF 0.5 4区 地球科学 Q4 GEOLOGY
L. Xiao
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引用次数: 8

摘要

Hecke轨道猜想对理解志村变异的几何结构起着重要的作用。Hecke轨道猜想首先由Chai和Oort于1995年提出,该猜想预测了Shimura品种的mod p约简上的素数-p Hecke对应表征了Oort中心叶形成的叶状结构。换句话说,每一个质数到p的赫克轨道在包含它的中心叶上都是扎里斯基密度的。粗略地说,中心叶是由对应Barsotti-Tate群属于固定几何同构类的所有点组成的Shimura变异中的轨迹。另一方面,闭点x的素数到p的Hecke轨道是由所有点y组成的(可数)集合,使得从x到y存在一个素数到p的拟同基因。2005年Chai和Yu证明了Hilbert模变的Hecke轨道猜想,同年Chai和Oort证明了Siegel模变的Hecke轨道猜想。本工作的主要目的是将Chai和Oort的方法推广到PEL型的Shimura品种。我们证明,在我们的假设下,赫克轨道猜想对牛顿地层中某些不可约分量中的点成立。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On The Hecke Orbit Conjecture for PEL Type Shimura Varieties
The Hecke orbit conjecture plays an important role in understanding the geometric structure of Shimura varieties. First postulated by Chai and Oort in 1995, the Hecke orbit conjecture predicts that prime-to-p Hecke correspondences on mod p reductions of Shimura varieties characterize the foliation structure formed by Oort's central leaves. In other words, every prime-to-p Hecke orbit is Zariski dense in the central leaf containing it. Roughly speaking, a central leaf is the locus in a Shimura variety consisting of all points whose corresponding Barsotti-Tate groups belong to a fixed geometric isomorphism class. On the other hand, the prime-to-p Hecke orbit of a closed point x is the (countable) set consisting of all points y such that there is a prime-to-p quasi-isogeny from x to y. In 2005, Chai and Yu proved the Hecke orbit conjecture for Hilbert modular varieties, followed by a proof for Siegel modular varieties by Chai and Oort in the same year. The major purpose of the present work is to generalize the method of Chai and Oort to Shimura varieties of PEL type. We show that the Hecke orbit conjecture holds for points in certain irreducible components of Newton strata under our assumptions.
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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