石油勘探与开发
石油勘探與開髮
석유감탐여개발
PETROLEUM EXPLORATION AND DEVELOPMENT
2001年
1期
45-47
,共3页
张庆春%石广仁%米石云%郭秋麟%杨秋琳
張慶春%石廣仁%米石雲%郭鞦麟%楊鞦琳
장경춘%석엄인%미석운%곽추린%양추림
土壤%地球化学勘探%指标%可靠性%烃类异常%油气远景%西藏%比如盆地
土壤%地毬化學勘探%指標%可靠性%烴類異常%油氣遠景%西藏%比如盆地
토양%지구화학감탐%지표%가고성%경류이상%유기원경%서장%비여분지
青藏高原是我国唯一没有进行大规模油气勘探的空白区,比如盆地的油气勘探程度更低。根据实际探测资料和试验数据,探讨地表地球化学勘探方法在青藏高原烃源岩大量出露地表的特殊条件下的有效性。研究表明,对于强风化的地表样品和灰岩裸露区,最有效的化探指标为甲烷和重烃浓度,其次为荧光和紫外光,而常用的蚀变碳酸盐指标应用效果不佳。比如盆地地表土壤中检测到的烃类主要来源于地下烃类的微渗漏,受生物活动的影响较小,化探结果能较真实地反映地下油气信息。比如盆地内有机质以高成熟和过成熟为主,主要处于生气阶段,地表地球化学异常较高,盆地中部异常最显著,凯蒙呷拉蒙地区具有一定的含油气远景,为油气勘探的有利区带。图3表2参1(程顶胜摘)
青藏高原是我國唯一沒有進行大規模油氣勘探的空白區,比如盆地的油氣勘探程度更低。根據實際探測資料和試驗數據,探討地錶地毬化學勘探方法在青藏高原烴源巖大量齣露地錶的特殊條件下的有效性。研究錶明,對于彊風化的地錶樣品和灰巖裸露區,最有效的化探指標為甲烷和重烴濃度,其次為熒光和紫外光,而常用的蝕變碳痠鹽指標應用效果不佳。比如盆地地錶土壤中檢測到的烴類主要來源于地下烴類的微滲漏,受生物活動的影響較小,化探結果能較真實地反映地下油氣信息。比如盆地內有機質以高成熟和過成熟為主,主要處于生氣階段,地錶地毬化學異常較高,盆地中部異常最顯著,凱矇呷拉矇地區具有一定的含油氣遠景,為油氣勘探的有利區帶。圖3錶2參1(程頂勝摘)
청장고원시아국유일몰유진행대규모유기감탐적공백구,비여분지적유기감탐정도경저。근거실제탐측자료화시험수거,탐토지표지구화학감탐방법재청장고원경원암대량출로지표적특수조건하적유효성。연구표명,대우강풍화적지표양품화회암라로구,최유효적화탐지표위갑완화중경농도,기차위형광화자외광,이상용적식변탄산염지표응용효과불가。비여분지지표토양중검측도적경류주요래원우지하경류적미삼루,수생물활동적영향교소,화탐결과능교진실지반영지하유기신식。비여분지내유궤질이고성숙화과성숙위주,주요처우생기계단,지표지구화학이상교고,분지중부이상최현저,개몽합랍몽지구구유일정적함유기원경,위유기감탐적유리구대。도3표2삼1(정정성적)
The Qinghai-Tibet Plateau is the only blank space of petroleum exploration in a large scale. Biru basin is much less explored. In this paper, according to the actually tested data and experiment results, the authors probed the efficiency for applying the surface geochemical exploration in Qinghai-Tibet Plateau, especially under the conditions of hydrocarbon source rocks being widely exposed. The research results indicate that, in the samples being strongly weathered or from the exposed limestone area, methane and heavy hydrocarbon content indices are of most valid, and then the fluorescence spectrum and ultraviolet spectrum indices, but altered carbonate index is not valid. In Biru basin, the hydrocarbons being detected in soil are mainly sourced from underground hydrocarbons by micro-leakage, and they are less affected by biological activity, which shows that geochemical results can really reflect the hydrocarbon information underground. The organic matter are high mature or overmature and at the gas-generating stage. In Biru basin, there occurs high surface geochemical abnormality, especially in the center of the basin. Kemenxialamen area is the hydrocarbon prospect area.