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Table 3 Detected model parameters, apparent chargeability, and volume fraction of conductive metal sulfides

From: Correlation between induced polarization and sulfide content of rock samples obtained from seafloor hydrothermal mounds in the Okinawa Trough, Japan

ID

\({\phi }_{m}\)

\({{\text{log}}}_{10}F\)

\(m\)

\({{\text{log}}}_{10}{\rm T}\)

\(c\)

RMSLE

\({{\text{log}}}_{10}{F}_{ave}\)

\({m}_{{\text{ave}}}\)

\({{\text{log}}}_{10}{\rm T}_{{\text{ave}}}\)

\({c}_{{\text{ave}}}\)

Average RMSLE for individual CCM

\(m^{\prime}\)(apparent)

[\(\bullet\)]

[\(\bullet\)]

[\(\bullet\)]

[\({{\text{Sm}}}^{-1}{\text{s}}\)]

[\(\bullet\)]

[\(\bullet\)]

[\(\bullet\)]

[\({{\text{Sm}}}^{-1}{\text{s}}\)]

[\(\bullet\)]

[\(\bullet\)]

KM18-08C #79 R01A

0.007

1.188

0.436

− 7.50

0.429

0.319

1.193

0.549

− 8.22

0.345

0.213

0.135

KM18-08C #79 R01B

0.006

1.150

0.453

-7.40

0.362

0.229

1.154

0.530

− 8.22

0.298

0.115

0.163

KM18-08C #79 R01C

0.006

1.302

0.560

− 7.24

0.465

0.242

1.289

0.617

− 8.22

0.370

0.118

0.195

KM18-08C #81 R01_1

0.062

0.609

0.587

− 5.14

0.338

0.303

0.724

0.726

− 6.96

0.210

0.047

0.452

KM18-08C #81 R01_2

0.042

0.855

0.628

− 5.45

0.296

0.210

0.882

0.660

-6.04

0.231

0.040

0.428

KM18-08C #81 R02

0.077

0.794

0.925

− 3.10

0.355

0.691

3.585

1.000

− 3.44

0.201

0.118

0.733

KM18-08C #84 R04A 3

0.170

1.558

0.993

-3.63

0.497

0.199

2.257

0.995

− 3.64

0.434

0.076

0.955

KM18-08C #84 R04A 4

0.069

1.161

0.948

-3.92

0.387

0.516

3.244

0.996

− 4.00

0.239

0.055

0.840

KM18-08C #84 R04B 1

0.081

1.285

0.906

− 5.00

0.397

0.357

1.719

0.945

− 6.89

0.217

0.022

0.791

KM18-08C #84 R04B 2

0.099

1.222

0.918

− 4.59

0.382

0.305

1.771

0.965

− 6.12

0.214

0.027

0.821

KM18-08C #84 R04B 3

0.086

1.200

0.948

− 3.84

0.331

0.383

3.541

0.999

− 4.52

0.208

0.033

0.808

KM18-08C #84 R04B 4

0.084

1.245

0.913

− 4.54

0.311

0.339

2.374

0.976

− 5.77

0.177

0.025

0.768

KM18-08C #84 R04B 5

0.106

1.123

0.883

− 4.77

0.331

0.277

1.328

0.947

− 6.54

0.187

0.034

0.769

KM18-08C #85 R01_1

0.413

2.489

0.999

− 1.62

0.347

0.223

2.624

0.993

− 1.44

0.359

0.109

0.722

KM18-08C #85 R01_2

0.425

3.026

1.000

-0.89

0.308

0.186

3.541

1.000

− 0.67

0.310

0.121

0.491

YK16-12 6 K# 1471 R01_1-1

0.024

0.571

0.514

− 5.63

0.374

0.274

0.675

0.641

− 8.40

0.170

0.165

0.262

YK16-12 6 K# 1471 R01_2-1

0.020

0.842

0.548

-6.24

0.391

0.284

0.920

0.621

− 8.40

0.233

0.169

0.217

YK16-12 6 K# 1471 R01_2-2

0.027

0.941

0.659

-5.87

0.354

0.352

1.146

0.702

− 8.11

0.145

0.189

0.340

YK16-12 6 K# 1471 R01_3-1

0.006

0.572

0.397

− 6.24

0.400

0.264

0.666

0.454

− 7.85

0.256

0.224

0.149

YK16-12 6 K# 1471 R01_3-2

0.003

0.217

0.231

− 6.19

0.391

0.315

0.330

0.320

− 7.89

0.218

0.244

0.091

YK16-12 6 K# 1471 R02_1-1

0.224

0.224

0.817

− 2.82

0.300

0.259

2.330

0.948

− 1.70

0.264

0.129

0.635

YK16-12 6 K# 1471 R02_2-1

0.139

0.010

0.789

− 3.19

0.365

0.274

1.647

0.894

− 2.24

0.298

0.158

0.621

YK16-12 6 K# 1471 R02_3-1

0.344

7.9E-06

0.894

− 2.06

0.355

0.162

1.735

0.894

-1.87

0.395

0.194

0.665

YK16-12 6 K# 1471 R02_4-1

0.42

7.5E-08

0.904

− 2.05

0.363

0.175

0.816

0.832

− 2.04

0.422

0.191

0.669