Table 3 Data of fluid inclusions, clumped isotopes and U-Pb ages from Ediacaran to ordovician in Tarim basin.

From: Using Mg isotopes to constrain the formation temperature of dolomite

Types

Formation

Fluid inclusions

Clumped isotopes thermometer

U-Pb age

D1

Qigebuklake

–

30 °C~32 °C 23

576 ± 16 Ma 23

D1

Qigebuklake

–

51 °C 24

560 ± 26 Ma 23

D2

Xiaoerbulake

70 °C~110 °C 25

–

491.6 ± 9.2 Ma or 488 ± 24Ma 26

D3

Penglaiba

119.8 °C ~ 170.9 °C 27

–

433 ± 22 Ma to 382 ± 29Ma 75

D3

Yingshan

–

94 °C~111 °C 28

464 ± 12 Ma 28,76

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