Here is some more info on attempts to trace the changing Earth-Moon distance and Earth's LOD back through geologic time, some tables go to 3.2 Gyr in Precambrian strata. However, the introduction does indicate that geologic strata used to interpret and reconstruct this past orbital history, is difficult to validate.
The Resonant Tidal Evolution of the Earth-Moon Distance,
https://arxiv.org/abs/2207.00438
Ref -
https://arxiv.org/pdf/2207.00438.pdf, 04-July-2022, 20-page PDF report, see attached. “1. Introduction Due to the tidal interplay in the Earth-Moon system, the spin of the Earth brakes with time and the Earth-Moon distance increases (Darwin 1879) at a present rate of 3.830 +/-0.008 cm/year that is measured using Lunar Laser Ranging (LLR) (Williams & Boggs 2016). There exists a rich narrative exploring the long term evolution of the system (Goldreich 1966; Mignard 1979; Touma&Wisdom 1994; Neron de Surgy& Laskar 1997) and the dynamical constraints on the origin of the Moon (Touma &Wisdom 1998; C´ uk et al. 2019). Among all, it has been established that simple tidal models starting with the present recession rate and integrated backward in time predict a close encounter in the Earth-Moon system within less than 1.6 billion years (Ga) (Gerstenkorn 1967; MacDonald 1967). This is clearly not compatible with the estimated age of the Moon of 4.425 +/- 0.025 Ga (Maurice et al. 2020), which suggests that the present rate of rotational energy dissipation is much larger than it has typically been over the Earth’s history. To bypass this difficulty, empirical models have been fitted to the available geological evidences of the past rotational state of the Earth (Walker & Zahnle 1986; Waltham 2015), acquired through the analysis of paleontological data (e.g. (Williams 2000)), sedimentary records of tidal rhythmites (Williams 1997; Sonett & Chan 1998; Williams 2000; Eriksson & Simpson 2000; de Azarevich & Azarevich 2017), or Milankovitch cyclostratigraphic sequences (Meyers & Malinverno 2018; Huang et al. 2020; Sørensen et al. 2020; Lantink et al. 2021). However, such models bring very little physical insight, and the remaining uncertainty of the geological data itself does not prevent circular arguments”.
My observation. This is refreshing to read and indicates the geologic record used to argue for the rate of change in Earth's rotation, lunar distance, etc. is difficult to use at best and we have an age for the Earth-Moon system < 1.6 Gyr old if current lunar recession rate or tidal dissipation rate used throughout geologic time. There are good tables in the PDF report like Table D.1. and Table D.2. Extrapolations for Earth-Moon distance and LOD for Earth too. 2.46 Gyr the distance is 50.24 earth radii and Earth LOD 16.98-hour day. Another value is 3.2 Gyr with Earth-Moon distance 46.45 earth radii compared to mean today about 60.27 earth radii with Earth LOD 15.17-hour day. At 46.45 earth radii, the Moon's angular size is larger than 40 arcminutes.
I searched the 20-page PDF for Theia and giant impact model, did not find references. The giant impact model takes place with a proto-earth and Theia, resulting in a proto-Earth with proto-Moon forming, both continue to accrete and grow

Some reports I have indicate the early Moon formed some 4-6 earth radii distance in the giant impact model compared to mean today near 60.27 earth radii. Such a distance would provide an angular size for the early Moon, assuming same diameter as today about 5.18 degrees across.
However, using my telescopes today, I cannot verify these orbital changes in the Earth-Moon system extrapolated back through geologic time

. Such orbital changes and LOD for Earth are significant.