Oil & Gas Geology ›› 2021, Vol. 42 ›› Issue (3): 639-651.doi: 10.11743/ogg20210310
• Petroleum Geology • Previous Articles Next Articles
Ting Li1,2(), Dancheng Zhu1,2, Minglei Yang1,2, Pingping Li1,2, Huayao Zou1,2,*()
Received:
2020-12-30
Online:
2021-06-28
Published:
2021-06-23
Contact:
Huayao Zou
E-mail:cuperliting@163.com;huayaozou@cup.edu.cn
CLC Number:
Ting Li, Dancheng Zhu, Minglei Yang, Pingping Li, Huayao Zou. Influence of hydrothermal activity on the Maokou Formation dolostone in the central and western Sichuan Basin[J]. Oil & Gas Geology, 2021, 42(3): 639-651.
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Table 1
Carbon and oxygen isotopes, strontium isotopes, Fe and Mn contents of limestone and different types of dolostone in the Maokou Formation, Sichuan Basin"
样品来源 | 岩性 | 层位 | 宏观产状 | 微观结构 | 晶体形态 | 晶体分布 | δ18O(PDB)/‰ | δ13C(PDB)/‰ | 87Sr/86Sr | Fe/10-6 | Mn/10-6 |
丰都放牛坝剖面 | 白云岩 | 茅三段 | 层状 | 粉-细晶 | 自形 | 单峰 | -3.3 | 4.3 | 0.707 701 | 268.1 | 22.0 |
白云岩 | 茅三段 | 层状 | 粉-细晶 | 自形 | 单峰 | -4.2 | 4.1 | 0.707 823 | 382.8 | 36.1 | |
白云岩 | 茅三段 | 层状 | 中晶 | 它形 | 单峰 | -7.2 | 3.4 | 0.707 935 | 1 243.8 | 69.9 | |
白云岩 | 茅三段 | 胶结物 | 鞍状晶 | 它形 | — | -10.9 | 4.0 | 0.710 186 | 1 145.4 | 127.6 | |
白云岩 | 茅三段 | 斑块状 | 中-粗晶 | 半自形 | 多峰 | -9.3 | 4.2 | 0.709 122 | 2 235.7 | 98.9 | |
泥晶灰岩 | 茅三段 | — | — | — | — | -4.6 | 3.8 | 0.707 384 | 135.0 | 21.0 | |
华蓥二崖剖面 | 白云岩 | 茅二段 | 层状 | 细-中晶 | 半自形-自形 | 多峰 | -7.2 | 3.2 | 0.707 975 | 861.7 | 59.6 |
白云岩 | 茅二段 | 层状 | 细-中晶 | 半自形-自形 | 多峰 | -6.8 | 3.8 | 0.707 838 | 457.1 | 49.1 | |
白云岩 | 茅二段 | 斑块状 | 中-粗晶 | 它形 | 单峰 | -11.6 | 3.3 | 0.709 328 | 1 971.4 | 180.0 | |
白云岩 | 茅二段 | 胶结物 | 鞍状晶 | 它形 | — | -11.4 | 3.9 | 0.709 595 | 1 006.0 | 180.1 | |
泥晶灰岩 | 茅二段 | — | — | — | — | -4.1 | 4.2 | 0.707 095 | 258.8 | 39.3 | |
泰来6井 | 白云岩 | 茅三段 | 层状 | 细-中晶 | 半自形 | 多峰 | -7.6 | 3.1 | 0.708 167 | 319.4 | 57.7 |
白云岩 | 茅三段 | 胶结物 | 鞍状晶 | 它形 | — | -9.8 | 2.9 | 0.708 236 | 1 099.1 | 136.2 | |
白云岩 | 茅三段 | 层状 | 粉晶 | 自形 | 单峰 | -3.9 | 4.2 | 0.707 508 | 316.7 | 46.3 | |
泥晶灰岩 | 茅三段 | — | — | — | — | -5.0 | 3.9 | 0.707 403 | 165.2 | 9.8 | |
邻水大坪剖面 | 白云岩 | 茅二段 | 层状 | 粉晶 | 自形 | 单峰 | -4.9 | 3.6 | 0.707 702 | 283.7 | 28.6 |
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