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Table 1 P–T–t conditions and estimated values of kinetic parameters for the back-transformation from ringwoodite to olivine

From: Back-transformation processes in high-pressure minerals: implications for planetary collisions and diamond transportation from the deep Earth

Run No.

Pressure (GPa)

Temperature (°C)

Duration (s)

∆Gr (J/mol)

n

ln k

Growth rate1 (m/s)

M2932

0.5

715

360

− 45,101

0.67

− 4.36

3.0 (0.1) × 10–9

M2716

1.1

615

1620

− 41,382

No transformation

 

1.1

765

1225

− 43,039

0.64

− 1.96

5.7 (0.4) × 10–8

M2893

1.2

510

1055

− 39,817

No transformation

 

1.2

645

18,340

− 41,283

0.85

− 9.10

3.8 (0.1) × 10–11

M2614

1.3

920

135

− 43,924

Completed within 10 s

M2714

1.9

455

3920

− 36,326

No transformation

 

1.7

715

2720

− 39,917

0.89

− 6.74

7.2 (0.1) × 10–10

M2620

4.1

510

445

− 28,161

No transformation

 

4.1

820

230

− 31,202

1.11

− 3.50

5.8 (0.4) × 10–8

M2717

7.4

515

435

− 16,122

No transformation

M2096

7.5

700

415

− 17,412

No transformation

 

6.6

800

2590

− 21,536

0.91

− 5.63

2.9 (0.2) × 10–9

  1. 1The uncertainties in growth rate are listed in parentheses