Discovery of crested quasi-periodic eruptions following the most luminous SRG/eROSITA tidal disruption event

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Table C.1.

Results of the single-blackbody time-resolved spectral modeling of the XMM-Newton dataset.

	Comp.	Δt	kT₁	L_bol, 1	R_BB, 1
		[s]	[eV]	[10⁴³ erg/s]	[10¹¹ cm]
E-1	a	414	$50_{- 6}^{+ 7}$ $50^{+7}_{-6}$	$2 . 18_{- 0.76}^{+ 1.15}$ $2.18^{+1.15}_{-0.76}$	5.1 ± 1.8
	b	378	$44_{- 9}^{+ 12}$ $44^{+12}_{-9}$	$2 . 56_{- 1.57}^{+ 3.31}$ $2.56^{+3.31}_{-1.57}$	7.4 ± 5
	c	540	$68_{- 4}^{+ 5}$ $68^{+5}_{-4}$	$3 . 18_{0.42}^{0.48}$ $3.18^{0.48}_{0.42}$	3.4 ± 0.5
	d	648	57 ± 4	$2 . 61_{- 0.51}^{+ 0.62}$ $2.61^{+0.62}_{-0.51}$	4.3 ± 0.8
	e	1080	$44_{- 5}^{+ 6}$ $44^{+6}_{-5}$	$1 . 86_{- 0.68}^{+ 1}$ $1.86^{+1}_{-0.68}$	6.1 ± 2.1

F-1	a	693	$68_{- 10}^{+ 11}$ $68^{+11}_{-10}$	$0 . 61_{- 0.18}^{+ 0.25}$ $0.61^{+0.25}_{-0.18}$	1.5 ± 0.5

F-2	b	747	$58_{- 6}^{+ 7}$ $58^{+7}_{-6}$	$1 . 45_{- 0.36}^{+ 0.47}$ $1.45^{+0.47}_{-0.36}$	3.2 ± 0.8

E-2	a	189	$146_{- 1}^{+ 13}$ $146^{+13}_{-1}$	$2 . 18_{0.21}^{0.23}$ $2.18^{0.23}_{0.21}$	0.6 ± 0.1
	b	237	$80_{- 17}^{+ 23}$ $80^{+23}_{-17}$	$0 . 55_{- 0.21}^{+ 0.32}$ $0.55^{+0.32}_{-0.21}$	1 ± 0.6
	c	329	$95_{- 5}^{+ 5}$ $95^{+5}_{-5}$	$3 . 61_{0.31}^{0.33}$ $3.61^{0.33}_{0.31}$	1.8 ± 0.2
	d	306	71 ± 7	$2 . 39_{- 0.47}^{+ 0.54}$ $2.39^{+0.54}_{-0.47}$	2.7 ± 0.6
	e	252	84 ± 5	$3_{0.39}^{0.43}$ $3^{0.43}_{0.39}$	2.1 ± 0.3
	f	738	64 ± 4	$1 . 31_{- 0.21}^{+ 0.23}$ $1.31^{+0.23}_{-0.21}$	2.5 ± 0.4
	g	739	$56_{- 6}^{+ 7}$ $56^{+7}_{-6}$	$1 . 01_{- 0.3}^{+ 0.44}$ $1.01^{+0.44}_{-0.3}$	2.8 ± 0.8

E-3	a	110	$102_{- 10}^{+ 12}$ $102^{+12}_{-10}$	1.25 ± 0.24	0.9 ± 0.2
	b	356	$109_{- 23}^{+ 30}$ $109^{+30}_{-23}$	0.81 ± 0.20	0.7 ± 0.3

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