本文選題：哈薩克斯坦 + Marsel探區(qū)�。� 參考：《古地理學(xué)報(bào)》2017年05期

【摘要】：根據(jù)Gr值、TH/U值和成像測(cè)井等測(cè)井資料,以及巖心、薄片等反映沉積基準(zhǔn)面和沉積相變化的資料,在哈薩克斯坦Marsel探區(qū)下石炭統(tǒng)碳酸鹽巖臺(tái)地內(nèi)劃分出18個(gè)高頻層序(四級(jí)層序),其中杜內(nèi)階和維憲階高頻層序界面類型主要為瞬時(shí)加深淹沒(méi)間斷面,謝爾普霍夫階高頻層序界面類型主要為瞬時(shí)暴露間斷面。高頻層序一般厚十幾米至幾十米,杜內(nèi)期—維憲早期厚度較薄且差異不大,維憲中晚期—謝爾普霍夫期厚度差異增大,最終使下石炭統(tǒng)整體呈西薄東厚、北薄南厚的特征。杜內(nèi)—維憲早期高頻層序下部主要發(fā)育蒸發(fā)o_湖和局限o_湖亞相,上部主要為局限潮坪亞相;維憲中晚期—謝爾普霍夫期高頻層序下部主要發(fā)育局限潮坪亞相,向上變?yōu)檎舭l(fā)潮坪和臺(tái)內(nèi)淺灘亞相。通過(guò)對(duì)高頻層序的成因分析認(rèn)為,周期性高頻海平面升降變化和氣候是高頻層序發(fā)育的主控因素,氣候?qū)S憲晚期—謝爾普霍夫期高頻層序發(fā)育的影響更大。Marsel探區(qū)在早石炭世位于鑲邊臺(tái)地內(nèi)部,先后經(jīng)歷了早期(杜內(nèi)期)局限臺(tái)地—蒸發(fā)臺(tái)地、中期(維憲期)局限臺(tái)地—蒸發(fā)臺(tái)地和晚期(謝爾普霍夫期)開闊臺(tái)地—局限臺(tái)地—蒸發(fā)臺(tái)地這3期沉積演化過(guò)程。高頻層序的研究為建立高精度層序地層格架和有利儲(chǔ)集層的精細(xì)劃分、對(duì)比及預(yù)測(cè)奠定了基礎(chǔ)。
[Abstract]:According to the values of Gr, TH- / U, imaging logging and other logging data, as well as the core, thin slice and other data reflecting the change of sedimentary datum and sedimentary facies, In the lower Carboniferous carbonate platform of Marsel exploration area, Kazakhstan, 18 high-frequency sequences (Quadrature sequence) have been divided, in which the interfacial types of high-frequency sequences of Dune and Weixian are mainly instantaneous deepening submerged discontinuities. The main types of high frequency sequence interface in the Scherphoff order are transient exposure intersections. The high frequency sequence is usually more than 10 meters to several tens meters thick, and the thickness of the Dune period to the early stage of Weixian is thin and the difference is small, and the thickness difference of the middle and late period of the Weixian to the Sherphoff period increases, which finally makes the lower Carboniferous series as a whole with a thickness of west thin east and north south thick. The lower part of the high frequency sequence mainly developed evaporative olake and limited olake subfacies, the upper part was mainly confined tidal flat subfacies, and the lower part of the high frequency sequence mainly developed limited tidal flat subfacies in the middle and late period of Weixian to Scherphoff period, and the lower part of the high frequency sequence in the middle and late period of Weixian developed limited tidal flat subfacies. Up to the evaporative tidal flat and subfacies of the shoal in the platform. By analyzing the cause of formation of high frequency sequence, it is concluded that periodic high frequency sea level fluctuation and climate are the main controlling factors for the development of high frequency sequence. The influence of climate on the development of high-frequency sequences in the late Weixian and Schaphov period is greater. The Marsel exploration area is located in the edge terrace in the early Carboniferous, and has experienced the early stage (Dune period) limited platform and evaporation platform, and the Marsel exploration area is located in the early Carboniferous. The sedimentary evolution processes of the three periods are limited platform-evaporation platform and late stage (Shephov period) open platform-limited platform-evaporation platform. The study of high-frequency sequences lays a foundation for the establishment of high-precision sequence stratigraphic framework and the fine division, correlation and prediction of favorable reservoirs.
【作者單位】： 中國(guó)地質(zhì)大學(xué)(北京)能源學(xué)院;中國(guó)地質(zhì)大學(xué)(北京)海洋學(xué)院;洲際油氣股份有限公司;
【基金】：國(guó)家重點(diǎn)基礎(chǔ)研究發(fā)展計(jì)劃(973)項(xiàng)目(編號(hào):2011CB201100-03) 中央高�；究蒲袠I(yè)務(wù)費(fèi)專項(xiàng)資金(編號(hào):2652015362)聯(lián)合資助~~
【分類號(hào)】：P618.13

【相似文獻(xiàn)】

相關(guān)期刊論文 前10條

1 柳祖漢,李有禹,雷躍冬,陳代釗;澧縣羊耳山地區(qū)有無(wú)下石炭統(tǒng)[J];湘潭礦業(yè)學(xué)院學(xué)報(bào);1986年01期

2 嚴(yán)幼因;下?lián)P子區(qū)下石炭統(tǒng)[J];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所所刊;1987年02期

3 陳松;曾勇;王茵;王占磊;;安徽巢北地區(qū)下石炭統(tǒng)巖石微相特征[J];中國(guó)煤田地質(zhì);2007年03期

4 盧宏金;桂中北部地區(qū)下石炭統(tǒng)發(fā)現(xiàn)海參化石[J];廣西地質(zhì);1992年03期

5 金松橋;;甘肅北山區(qū)下石炭統(tǒng)劃分及其對(duì)比[J];地質(zhì)學(xué)報(bào);1974年02期

6 施希德;;柴達(dá)木東北緣阿木尼克山杜內(nèi)階的發(fā)現(xiàn)—兼對(duì)歐龍布魯克下石炭統(tǒng)劃分的討論[J];青海地質(zhì);1979年01期

7 嚴(yán)幼因;下?lián)P子區(qū)下石炭統(tǒng)底部陳家邊組簡(jiǎn)介[J];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所所刊;1987年01期

8 王瑞剛;象州縣崖腳下石炭統(tǒng)剖面簡(jiǎn)介[J];廣西地質(zhì);1996年03期

9 張良;;關(guān)于華南下石炭統(tǒng)建階問(wèn)題的討論[J];中國(guó)地質(zhì)科學(xué)院成都地質(zhì)礦產(chǎn)研究所文集;1985年00期

10 吳祥和,季強(qiáng),陳笑媛;揚(yáng)子地臺(tái)西南緣下石炭統(tǒng)中間界線地層[J];地層學(xué)雜志;1997年04期

相關(guān)會(huì)議論文 前6條

1 嚴(yán)幼因;;下?lián)P子區(qū)下石炭統(tǒng)[A];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所文集（28）[C];1987年

2 張良;;關(guān)于華南下石炭統(tǒng)建階問(wèn)題的討論[A];中國(guó)地質(zhì)科學(xué)院成都地質(zhì)礦產(chǎn)研究所文集（6）[C];1985年

3 嚴(yán)幼因;;下?lián)P子區(qū)下石炭統(tǒng)底部陳家邊組簡(jiǎn)介[A];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所文集（27）[C];1987年

4 張瑛;陳宏明;魏乃頤;張建勝;賀立民;;安徽巢湖地區(qū)下石炭統(tǒng)沉積特征[A];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所文集（10）[C];1983年

5 陳華成;王云慧;;蘇浙皖地區(qū)上、下石炭統(tǒng)之間白云巖的時(shí)代歸屬[A];中國(guó)地質(zhì)科學(xué)院南京地質(zhì)礦產(chǎn)研究所文集（13）[C];1984年

6 楊宗仁;;云南保山地區(qū)石炭系的劃分[A];青藏高原地質(zhì)文集（11）——“三江”地層、古生物[C];1982年

相關(guān)博士學(xué)位論文 前2條

1 周曉東;吉林省中東部地區(qū)下石炭統(tǒng)—下三疊統(tǒng)地層序列及構(gòu)造演化[D];吉林大學(xué);2009年

2 李宇平;輪南低凸起—哈得遜周緣下石炭統(tǒng)層序地層學(xué)研究與地層巖性油氣藏形成條件[D];西南石油大學(xué);2005年

相關(guān)碩士學(xué)位論文 前1條

1 韋樂(lè)樂(lè);羌南下石炭統(tǒng)日灣擦卡組古地磁研究[D];西北大學(xué);2015年

，

本文編號(hào)：2006529