Table 2 Homogenization temperature of fluid inclusions from different mineralization stages of the Weilasituo Sn-W-Li deposit.

From: Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China

Sample

Stage

Mineral

Type (n)

tm–ice/(-°C)

th-tot/°C

w(NaClep)/%

Range

Mean

Range

Mean

WL-13

I

Qz

L(21)

6.1–9.8

304–379

325

9.3–13.7

11.9

WL-15

I

Qz

L(14)

3.5–4.2

268–325

295

5.7–6.7

6.3

WL-16

I

Qz

L(30)

3.2–6.8

254–372

309

5.3–10.2

7.5

WL-27

I

Qz

L(13)

3.1–4.5

337–374

355

5.1–7.2

6.5

WL-40

I

Qz

L(17)

1.6–2.9

242–358

326

2.7–4.8

3.4

WL-49

I

Qz

L(10)

2.1–2.4

240–326

298

3.5–4.0

3.9

NW-Y-95

I

Qz

L(11)

4.2–4.8

226–297

270

6.7–7.6

7.1

NWN-125

III

Qz

L(26)

3.2–4.4

224–309

260

5.3–7.0

6.2

WL-21

III

Qz

L(25)

2.3–5.1

208–310

263

3.9–8.0

5.6

NWN-123

III

Qz

L(7)

2.6–3.6

337–367

352

4.3–5.9

4.8

WL-41

III

Qz

L(17)

2.4–3.4

303–334

315

4.0–5.6

4.6

NWN-121

IV

Qz

L(12)

2.0–4.8

223–265

255

3.4–7.6

5.3

NW-Y-12

IV

Qz

L(8)

1.6–3.3

236–258

249

2.7–5.4

4.2

WL-45

IV

Qz

L(17)

1.7–2.9

198–274

224

2.9–4.8

3.6

WL-46

IV

Qz

L(44)

1.6–2.9

176–288

250

2.7–4.8

3.8

NWN-127

IV

Qz

L(10)

1.3–2.7

224–317

241

2.2–4.4

4.2

WL-24

IV

Qz

L(14)

1.7–2.3

176–243

210

2.9–3.9

3.0

WQ-5

WQ-5Rim

Qz

L(14)

2.8–3.9

251–272

260

4.7–6.3

5.5

WQ-5

WQ-5Core

Qz

L(13)

3.4–3.9

264–336

284

5.6–6.3

6.0

  1. n, the number of fluid inclusions.