松辽盆地现今岩石圈热结构特征及主控因素

代登亮; 王守志; 边远; 王鹏; 刘宗堡; 赵容生

doi:10.19509/j.cnki.dzkq.tb20230609

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松辽盆地现今岩石圈热结构特征及主控因素

更新时间：2026-11-05

- 松辽盆地现今岩石圈热结构特征及主控因素
- Bulletin of Geological Science and Technology Vol. 44, Issue 5, Pages: 135-143(2025)
- 作者机构：
  
  1. 长春工程学院
  2. 长庆油田长庆实业集团有限公司
  3. 吉林省第一地质调查所
  4. 中国石油塔里木油田分公司
  5. 东北石油大学地球科学学院
  6. 吉林大学地球科学学院
- 作者简介：
- 基金信息：
- DOI：10.19509/j.cnki.dzkq.tb20230609
  CLC： P541;P31
- Online First：26 November 2024，
  
  Published：2025
- 稿件说明：
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代登亮, 王守志, 边远, et al. 松辽盆地现今岩石圈热结构特征及主控因素[J]. Bulletin of Geological Science and Technology, 2025, 44(5): 135-143.
DOI：

代登亮, 王守志, 边远, et al. 松辽盆地现今岩石圈热结构特征及主控因素[J]. Bulletin of Geological Science and Technology, 2025, 44(5): 135-143. DOI： 10.19509/j.cnki.dzkq.tb20230609.

摘要

松辽盆地的热结构分析多局限在南北分区的沉积层尺度，缺乏岩石圈尺度的全盆地热结构刻画，制约了以地球动力学为背景的成因分析。综合利用已发表的地表热流、地温梯度以及热物性参数，补充了姚家组、青山口组和泉头组的热物性测试分析，并增加了多个地温场数据，全面刻画了整个松辽盆地的地温场特征，剖析了现今岩石圈尺度的热结构特征。结果表明，松辽盆地地温梯度范围为21.10～63.45℃/km，平均值为（41.41±7.97）℃/km，高于全球平均的地温梯度值30℃/km；地表热流值的分布范围为30.38～106.58 mW/m

，平均值为（71.85±12.87） mW/m

，也高于全球平均的地表热流值60 mW/m

，是一个典型的“热”盆。受太平洋板块俯冲作用、拆沉作用和热侵蚀作用的影响，热岩石圈明显减薄至现今的58.59 km。由减薄地壳中放射性元素生热产生的热流仅为16.40 mW/m

，占地表热流的22.83%；而受滞留板片脱水作用的影响，部分熔融的地幔热物质上涌，地幔热流贡献高达55.45 mW/m

，占地表热流的77.17%。因此，受控于岩石圈减薄作用和地幔上涌作用，松辽盆地具有“热”盆属性和“热幔冷壳”的岩石圈热结构特征。

Abstract

ObjectivePrevious thermal structure analyses in the Songliao Basin have predominantly focused on the sedimentary scale investigations within the north-south zone. The lack of a comprehensive basin-wide thermal structure analysis at the lithospheric scale has hindered the genetic interpretation of its geodynamic setting. MethodsUtilizing published datasets of surface heat flow

geothermal gradient

and thermophysical properties

this study enhances the existing framework by incorporating new thermophysical measurements from the Yaojia Formation

Qingshankou Formation and Quantou Formation. Supplementary geothermal filed datasets were integrated to establish a holistic characterization of the basin's geothermal regime. This multi-scale approach enables systematic analysis of the contemporary lithospheric thermal architecture. ResultsThe results reveal that the geothermal temperature gradient in the Songliao Basin ranges from 21.10 to 63.45°C/km

with an average of 41.41±7.97°C/km

significantly exceeding the global average of 30°C/km. The distribution of surface heat flow values ranges from 30.38 to 106.58 mW/m2

with an average of 71.85±12.87 mW/m2

surpassing the global average of 60 mW/m2

confirming the basin as a typical "hot" basin. Under the influence of Pacific plate subduction

delamination and thermal erosion

the lithosperic thickness have thinned to 58.59 km. Radiogenic heat production in the thinned crust contributes 16.40 mW/m2 (22.83% of total surface heat flow)

while mantle-derived heat flow from upwelling melts triggered by stagnant slab dehydration accounts for 55.45 mW/m2 (77.17% of total) ConclusionControlled by lithospheric thinning and mantle upwelling

the Songliao Basin exhibits characteristic of "hot" basin attributues with a "hot mantle and cold crust" lithospheric thermal structure.

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