Fast magnetic reconnection is an explosive plasma process, bringing the topological reconfiguration of magnetic fields, plasma heating, and acceleration in laboratory and space plasmas (e.g., Gonzalez & Parker, 2016;Yamada et al., 2010). In general, this is a time-dependent multi-scale three-dimensional process (e.g., Bhattacharjee, 2004;Dorfman et al., 2013;Frank, 1999;Xiao et al., 2006), but sometimes reconnection may demonstrate a symmetric configuration and be quasi-stationary. Particularly, at the day side of the Earth's magnetopause, quasi-stationary reconnection has been detected in-situ on several occasions (e.g., Gosling et al., 1982;Phan et al., 2004;Retinò et al., 2005) as well as anti-parallel reconnection (Cassak & Fuselier, 2016, and references therein). The latter is more common in the Earth's magnetotail (Paschmann et al., 2013). It is also important that in many cases reconnection can be studied analytically in the frame of two-dimensional models for the considerable length of the reconnection X-line. Configurations with short X-lines demonstrate spreading in the X-line direction (see, e.g., Li et al., 2020, and references therein) in course of time. At last, both at the dayside magnetopause and in the magnetotail (e.g., Cassak &